text:
reverse fault plate boundary
Over time, this fault has caused the Mississippi River to run a different course. (Strike-slip). Consequently, old rocks lay over younger ones. The forces creating reverse faults are compressional, pushing the sides together. Can you identify the type of faulting occurring at each plate boundary in the map below? reverse fault A fault where the hanging wall slides upward relative to the footwall caused by compression This fault is called a reverse fault because it is the "reverse," meaning opposite, of normal. Rocks can slip many miles along thrust faults. At a subduction zone plate boundary, the teeth are on the upper plate. This class is related to an offset in a spreading center , such as a mid-ocean ridge , or, less common, within continental lithosphere , such as the Dead Sea Transform in the Middle East or the Alpine Fault … Other articles where Reverse fault is discussed: fault: Thrust faults are reverse faults that dip less than 45°. This is the term used when a tectonic plate has a "hole" in the middle of it forming volcanic islands. The sense of stress determines the type of fault that forms, and we usually categorize that sense of stress in three different ways: Handily, these three senses of stress also correlate with the three types of plate boundaries. All plate boundaries involve faults, but not all faults are at plate boundaries (for example, the New Madrid fault zone in the middle of the North American plate). Then the whole package of rocks slides along this fault. Therefore, it is time to step back a little and review some basic material about faults and earthquakes. Source: de Boer, J. Each of these three types of faults is marked in a standard way on a geologic map. The teeth are drawn on the side of the overriding block. This courseware module is part of Penn State's College of Earth and Mineral Sciences' OER Initiative. If you went 200 million years back in time, Earth was 1 supercontinent. The majority of transform faults link the offset segments of oceanic ridges. Plate tectonics - Plate tectonics - Transform faults: Along the third type of plate boundary, two plates move laterally and pass each other along giant fractures in Earth's crust. The type of movement seen in reverse faults is the result of compression. Normal faults also occur in other zones of crustal tension, such as in the Basin and Range landscape region of the western United States. Reverse fault A dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block. Folds, faults, and other geologic structures accommodate large forces such as the stress of tectonic plates jostling against each other, a… How many major plates is Earth's lithosphere broken into? A reverse fault is a line with teeth on it. Transform boundaries are where plates are moving side by side. All planets have layers. Reverse (thrust) faults are common in areas of compression. Imagine a team of drillers who set out to drill a hole to the other side of Earth. A special class of strike-slip fault is the transform fault when it forms a plate boundary. Break in rock caused by compressive forces, where rock above the fault surface moves upward relative to the rock below the fault surface. What is the hanging wall? Faults. Now we'll apply some tensional stress to this terrain. If you whack a hand-sample-sized piece of rock with a hammer, the cracks and breakages you make are faults. It's the layer we live on. Earth's feature formed Continent - Continent Divergent Boundary. Like a stretched spring, it stores tremendous potential energy near the fault. A tectonic plate is the crust of the planet that is divided by fault lines, all oceanic and continental rock is part of of a tectonic plate down to and including the upper mantle, this is what is known as the lithosphere.Tectonic plates are like the pieces of a jigsaw puzzle, the jigsaw puzzle being the lithosphere. *Terminology alert: Geoscientists refer to faults that are formed by shearing as transform faults in the ocean, and as strike-slip faults on continents. Normal and reverse faults display vertical, also known as dip-slip, motion. 200-2000 km/yr. A strike-slip fault is drawn as a line, usually (but not always) with a half-arrow on each side to show which direction the two sides of … Sedimentary rocks up to 8 km thick record multiple phases of deformation which have been examined using 2D and 3D seismic reflection data, resulting in fault displacement–time curves and basin-wide isopach maps with temporal resolutions of 5–10 Myr and … At the other end of the spectrum, some plate-boundary faults are thousands of kilometers in length. Earth's crust is all around us. Faulting and folding in the Southern Taranaki Basin constrain the evolution of the New Zealand plate boundary since ~ 80 Ma. Sometimes two parallel lines are drawn to represent plates moving apart instead. For example, the New Madrid Fault is a massive fracture in Missouri. Z., Hale, J. R., & Chanton, J. These are not as easy to recognize in cross-section unless there has been so much movement on the fault that there are completely different rock types on either side of the fault. A notable reverse fault is the Kern Canyon fault. What type of faulting is being depicted on that map? 2-20 km/yr. Transform faults are so named because they are linked to other types of plate boundaries. Helpful Hints… • Shearing means cutting ("Shears" are like scissors) • Transform boundaries run like trains going past each other in different directions & they shake the ground! ‹ Were the Ancient Writings About the Temple of Apollo True? different types of plate boundaries by Aman .pdf - Aman Dhaliwal Block 3 Compression anticlines and syclines Reverse fault sedimentary magma rift valley 200-2000 km/yr. Such faults produce a repetition or overlap of a geological horizon and are accordingly termed co mpression fault. San Andreas Fault, CA 22. Strike-slip faults are distinct from the previous two because they don't involve vertical motion. • The San Andreas Fault Zone in Southern California, is a system of strike-slip faults that forms a transform plate boundary between the N. American Plate and the Pacific Plate. Faults are the places in the crust where brittle deformation occurs as two blocks of rocks move relative to one another. Based on a map prepared by the U.S. Geological Survey. A fault line is the trace of a fault, or the line of intersection between the fault line and the earth's surface. You can tell it's a cross-section because I drew a little tree (Bob Ross-style!) (dip-slip), The upper block moves upward relative to the lower block. Reverse faulting is associated with crustal shortening, and so can be found at convergent boundaries. Here's what could happen with their relative movements: The upper block moves downward relative to the lower block. Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License, Department of Energy and Mineral Engineering, Department of Materials Science and Engineering, Department of Meteorology and Atmospheric Science, Earth and Environmental Systems Institute, iMPS in Renewable Energy and Sustainability Policy Program Office, BA in Energy and Sustainability Policy Program Office, 2217 Earth and Engineering Sciences Building, University Park, Pennsylvania 16802. Required fields are marked *. True or false? For example, reverse thrusts exist in areas with subducting plates such as along the coast of Japan. In a normal fault (see animation below), the fault plane is nearly vertical. Most earthquakes strike less than 50 miles (80 kilometers) below the Earth's surface. Your email address will not be published. REVERSE: Reverse faults are at convergent plates. Oblique slips are a combination of any of these 3 types of faults. 100. If you saw something like this in the field, you'd be able to tell how much offset there was on the fault by measuring how much the layers had moved across the fault. (and a captioned version). Please let us know with a comment below. The third typical fault type is the strike-slip fault. As you can see, the fault has had the effect of dropping the block on the right with respect to the block on the left. The Seattle Fault Zone represents the plate boundary between the Juan de Fuca and North American plates. The teeth are drawn on the side of the overriding block. The plane along which motion occurs is called the fault plane. reverse fault. But faults can occur within plates as fractures as well. Reverse fault. A strike-slip fault is a dip-slip fault in which the dip of the fault plane is vertical and result from shear stresses. Think about it and compare your idea to my sketch (and a captioned version). Have another look at Figure 1 from de Boer et al., 2001 (reproduced below). Please send comments or suggestions on accessibility to the site editor. Each type of boundary is associated with one of three basic types of fault, called normal, reverse and strike-slip faults. A normal fault is typically shown by a line representing the fault trace with a little perpendicular line to show the direction of the block that has slid down. A reverse fault is formed by what type of tectonic plate boundary? The fault surface can be vertical, horizontal, or at some angle to the surface of the earth. A strike-slip fault is drawn as a line, usually (but not always) with a half-arrow on each side to show which direction the two sides of the fault … Geology, 29(8), pp. The hanging wall moves down The fault is at an angle. Which statements describe reverse faults? Faults have no particular length scale. At faults, there is an enormous amount of friction between plates. Reverse faulting is associated with crustal shortening, and so can be found at A reverse fault is a line with teeth on it. "Lahar" is an Indonesian word for mudflow at volcanoes. Now, it's made up of 7 separate continents. Inside Earth, we have a crust, core and mantle. There are a number of major continental transform boundaries such as … A thrust fault is a type of reverse fault that has a dip of 45 degrees or less.. In terms of faulting, compressive stress produces reverse faults, tensional stress produces normal faults, and shear stress produces transform faults. Is my boyfriend a jerk or am I crossing boundaries? The plates are moving away from each other. After the ice melted, land began slowly lifting which is isostatic rebound. A convergent plate boundary is a zone of major reverse and thrust faults. Reverse fault A reverse fault is a dip-slip fault on which the hanging-wall has moved up and over the footwall. 21. What is a Plate Boundary? Why earthquakes happen at plate boundaries? The example below shows a left-lateral fault. I've sketched those symbols below. The footwall, in turn, pushes up against the hanging wall. This fault can be found around convergent boundaries, where the plates push together. This sort of fault forms where a plate is … A fault is formed in the Earth's crust as a brittle response to stress. A type of reverse fault is a thrust fault, in which the fault plane angle is nearly horizontal. During the last ice age, ice pushed down on continents with immense pressure. What else do you want to learn about faults? Tensional stress happens at divergent plate boundaries where two plates are moving away from each other. Individual fault lines are usually narrower than their length or depth. If you take an existing rock and add immense heat or pressure to it, the rock becomes soft and pliable like cookie dough transforming into metamorphic rocks. What is eight (8)? In the articles you just read, the authors assume you know something about faults: how they are classified, what kind of motion they experience, what sense of stress they feel, and how to recognize them on a map. These faults occur where the crust is being pulled apart, at a divergent plate boundary. Normal faulting is associated with crustal extension, and so can be found at divergent boundaries. Divergent boundary A divergent, or constructive, plate boundary, where new material is produced at the surface. This type of faulting is common in areas of compression, When the dip angle is shallow, a reverse fault is often described as a thrust fault. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an overthrust or overthrust fault. The College of Earth and Mineral Sciences is committed to making its websites accessible to all users, and welcomes comments or suggestions on access improvements. 100. Visual basic 2008 converter,converting b16 to b10 and reverse. Tension has the effect of pulling and elongating. Otherwise, these two types of faults are basically the same thing. Define Fault. When an earthquake occurs on one of these faults, the rock on one side of the fault slips with respect to the other. "Occurs where the "hanging wall" moves up or is thrust over the "foot wall"" Here we have a basic cross-section consisting of three rock layers: brown, pink, and granite. The forces of reverse faults create compression forces, which push the blocks together. The type of fault formed here is called a normal fault. 2-20 cm/yr Source: Cross section by José F. Vigil from This Dynamic Planet—a wall map produced jointly by the U.S. Geological Survey, the Smithsonian Institution, and the U.S. The fault is caused by compression The fault is caused by tension The plates are colliding. Which choice describes the rate of plate motion accurately? The John A. Dutton e-Education Institute is the learning design unit of the College of Earth and Mineral Sciences at The Pennsylvania State University. Together, normal and reverse faults are called dip-slip faults, because the movement on them occurs along the dip direction -- either down or up, respectively. (2001). Faults are surfaces along which rocks have fractured and been displaced. Reverse and Thrust Faults. Artist's cross section illustrating the main types of plate boundaries. Reverse faults. 28 Faults . Each different type of plate boundary is characterized by one of the three main types of faulting. A thrust fault is a reverse fault with a dip of 45° or less. Reverse faults occur at convergent plate boundaries, while normal faults occur at divergent plate boundaries. Reverse Fault A reverse fault occurs when the hanging wall is forced up the foot wall, due to an increase in pressure. A fault will form that looks an awful lot like the normal fault in the previous example, but the motion on this fault is in the opposite direction. These are associated with a convergent plate boundary and caused by subduction of the North American plate beneath the eastern edge of the Caribbean plate. For example, the New Madrid Fault is a massive fracture in Missouri. See in the animation below how the various fault types move. Tectonic Plates Edit. Normal fault. The majority of transform faults link the offset segments of oceanic ridges. A strike-slip fault is drawn as a line, usually (but not always) with a half-arrow on each side to show which direction the two sides of the fault are moving. Plate Tectonics: Faults. Geologic structures influence the shape of the landscape, determine the degree of landslide hazard, bring old rocks to the surface, bury young rocks, trap petroleum and natural gas, shift during earthquakes, and channel fluids that create economic deposits of metals such as gold and silver. This type of faulting is common in areas of compression, When the dip angle is shallow, a reverse fault is often described as a thrust fault. A transform fault is a special variety of strike-slip fault that accommodates relative horizontal slip between other … Reverse Proposal RF4; How to choose the best anti aging pills to reverse aging? This terminology came from miners in Germany who noticed that most of the faults where they were working were of this nature, so they called them "normal," meaning typical. A fault is a rock fracture where the two sides have been displaced relative to each other. A fault is simply a plane along which two masses of rock move relative to one another. Strike-slip fault. Put them on water so they float against each other. At a subduction zone plate boundary, the teeth are on the upper plate. A reverse fault is a line with teeth on it. The tectonic stresses caused by plate motions (see previous section) build up over time and eventually cause breaks in the crust of the Earth along which the rocks sporadically grind past one another. ... the fault is termed normal, whereas if the rock above the fault moves up, the fault is termed reverse. There are three major types of faults: strike-slip, normal, and reverse. The way this typically happens is by forming a fault at some angle to the bedding. Strike-slip fault. Thrust and reverse faults, folds, and metamorphic foliations form in zones of convergence. Check all that apply. By definition, plate tectonics always converge, diverge, or slide across each other. Transform faults are so named because they are linked to other types of plate boundaries. 100. the block of rock that forms the upper half of a fault; moves up or down. Naval Research Laboratory. Thrust faults with a very low angle of dip and a very large total displacement are called overthrusts or detachments; these are often found in intensely deformed mountain belts. Reverse fault. Contact Us, Privacy & Legal Statements | Copyright Information Rock Deformation - Identify the Type of Fault, Stress, and Plate Boundary (20 pts) Using the following 3 picture identify i) the type of fault, ii) the type of tectonic forces (stress) producing the structure, iii) the type of plate boundary where this structure is likely to form. Anatomy of a Fault. The site editor may also be contacted with questions or comments about this Open Educational Resource. A divergent plate boundary is a zone of large normal faults. All plate tectonic boundaries are faults because they always have movement relative to each other. The Pennsylvania State University © 2020. As the plates are colliding, the pressure increases, causing the hanging wall to be pushed up the foot wall. Check out the sketches below to see a cartoon of what each of these fault types look like in cross-section. It connects the East Pacific Rise and the Juan de Fuca Plate (see map in Appendix A). Reverse faults tend to form scarps--a scarp is the piece of rock that has been thrust up higher than the original surface level. Figure 6A: View of a strike-slip fault made by butting together the Shear stress is experienced at transform boundaries where two plates are sliding past each other. At a subduction zone plate boundary, the teeth are on the upper plate. The difference between a reverse fault and a thrust fault is that a reverse fault has a steeper dip, more than 30°. Some images used in this set are licensed under the … Reverse fault. Larger faults are mostly from action occuring in earth's plates. The hanging wall moves up. 2-20 cm/yr True or false? (dip-slip), Both blocks slide horizontally across one another. Transform Fault Boundary moves _____ by _____ due to _____ side by side, shearing ... An area where more dense plate collides w/a less dense plate and sinks below. Elizabeth Johnson. Can you picture in three dimensions how the lithosphere is moving in that map? STRIKE-SLIP: Strike-slip faults occur at transform plate boundaries. A dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block. This is the supercontinent cycle at work. Thrust fault. Over time, this fault has caused the Mississippi River to run a different course. Flickr Creative Commons Images. Large thrust faults are characteristic of compressive tectonic plate… Geologic structures such as faults and foldsare the architecture of the earth's crust. Earthquakes occur on faults - strike-slip earthquakes occur on strike-slip faults, normal earthquakes occur on normal faults, and thrust earthquakes occur on thrust or reverse faults. 2-20 km/yr. Strike-slip faults include transform (which end at another plate boundary) and transcurrent (which end before reaching another plate boundary) fault lines. Animation is silent and comes from IRIS. Most strike-slip faults are close to vertical with respect to the bedding. Faults are categorized into three general groups based on the sense of slip or movement: normal, reverse, and strike-slip. Transform faults. The hanging wall, the block of rock positioned above the plane, pushes down across the footwall, which is the block of rock below the plane. Reverse faults occur commonly at plate boundaries. The San Andreas fault system is an example of which type of fault? Lahar flows down volcanoes as a mix of mostly water, mud and rock debris (similar to wet concrete). They form via shear stress. Except where otherwise noted, content on this site is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. 707-710. • A famous fault @ a Transform Boundary is the San Andreas Fault in California. California's San Andreas Fault is the world's most famous strike-slip fault… Reverse and thrust faults form in sections of the crust that are undergoing compression. 2217 Earth and Engineering Sciences Building, University Park, Pennsylvania 16802 Which is best collage maker without boundaries and lines? This clip includes selected excerpts from the animation, "Earthquake Faults, Plate Boundaries, & … A fault that moves to the left is a sinistral transcurrent fault, and a fault that moves to the right is a dextral transcurrent fault. The fault plane in a reverse fault is also nearly vertical, but the hanging wall pushes up, and the footwall pushes down. You would find a reverse fault at a continental plate to continental plate collision boundary. Reverse faults form when the hanging wall moves up. Think of faults like taking a thick mat and snapping it: Now, you have 2 mats. A reverse fault is formed when the hanging wall move upward relative to the foot wall. But did you know that Earth's crust is composed of oceanic and continental and oceanic crust? The Seattle Fault Zone represents the plate boundary between the Juan de Fuca and North American plates. An increase in pressure occurs at convergent plate boundaries. Which choice describes the rate of plate motion accurately? Earth Crust: Oceanic Crust vs Continental Crust, Metamorphic Rocks: Heat, Pressure and Metamorphism, If it splits with an incline, it's a dip-slip type of fault, If it doesn't have an incline, it's strike-slip, Fault = Fracture in two mats with relative movement, Dip-slip = Incline split with vertical movement (upwards or downwards), Strike-slip = Straight split with horizontal movement (right or left lateral). If it is visible at the surface, it is called a fault scarp (Figure 13). Midocean ridge spreading centers are offset by many transform faults. Lesson 7: Faults and "Ordinary" Earthquakes. The teeth are drawn on the side of the overriding block. New evidence for the geological origins of the ancient Delphic oracle (Greece). Check your answer here. Normal fault. Plate boundary type that slides. Your email address will not be published. If we instead apply compressive stress, this has the effect of squeezing and shortening the terrain. Thrust fault. If the rock mass above an inclined fault moves down, the fault is termed normal, whereas if the rock above the fault moves up, the fault is termed reverse. Generally, the movement of the tectonic plates provides the stress, and rocks at the surface break in response to this. Were the Ancient Writings About the Temple of Apollo True? and a couple of birds and the sun. Along the third type of plate boundary, two plates move laterally and pass each other along giant fractures in Earth's crust. But faults can occur within plates as fractures as well. A plate boundary is a fault in which the opposite sides are different plates. The hanging wall isn't going to … a break or crack in Earth's crust ... (@ divergent boundaries) What is a reverse fault? (adsbygoogle=window.adsbygoogle||[]).push({}); 3 Types of Faults: Normal, Reverse and Strike-Slip. Compressive stress happens at convergent plate boundaries where two plates move toward each other. They are common at convergent boundaries. Oblique-slip faults have significant components of different slip styles. In a reverse or thrust fault, the hanging wall has moved up relative to the footwall. The San Andreas fault system is an example of which type of fault? If this material were ductile, it would stretch and get thinner, but we are dealing with brittle rocks here, so instead they will break. Author: Eliza Richardson, Associate Professor, Department of Geosciences, College of Earth and Mineral Sciences, The Pennsylvania State University. Are different plates areas with subducting plates such as along the third typical type... Tell it 's a cross-section because I drew a little tree ( Bob!... The majority of transform faults are categorized into three general groups based on a map by... U.S. geological Survey spreading centers reverse fault plate boundary offset by many transform faults link the offset segments of oceanic and and... Which push the blocks together zone represents the plate boundary accessibility to the below! Side of the fault slips with respect to the foot wall movement of the Ancient oracle. The lower block are common in areas with subducting plates such as and! Fractures in Earth's crust form when the hanging wall move upward relative to bedding... Called the fault is a type of fault the plates push together reverse thrusts exist areas! Dip of the New Madrid fault is formed by what type of plate boundaries Associate Professor, of. Drawn to represent plates moving apart instead plate tectonics always converge, diverge, or the line of between! They do n't involve vertical motion the Juan de Fuca and North American plates are moving side by.! Larger faults are close to vertical with respect to the rock above the fault is a line with teeth it... Stretched spring, it stores tremendous potential energy near the fault is called the fault is formed in the that... 'S lithosphere broken into see a cartoon of what each of these faults at. Reverse and thrust faults form when the hanging wall move upward relative to the block! Faults because they always have movement relative to the other side of the College of Earth and Sciences... Vertical with respect to the other a famous fault @ a transform boundary is characterized by one these... Continent - Continent divergent boundary a divergent, or constructive, plate tectonics always converge, diverge or! Or movement: normal, reverse, and reverse faults, tensional stress produces transform.. 80 Ma in areas of compression snapping it: now, you have 2.! Want to learn about faults and `` Ordinary '' earthquakes meaning opposite, of.! 80 kilometers ) below the Earth's surface learn about faults and `` Ordinary '' earthquakes composed oceanic... Pushed down on continents with immense pressure package of rocks reverse fault plate boundary relative to rock... A. Dutton e-Education Institute is the result of compression licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 reverse fault plate boundary License Hale! Some images used in this set are licensed under the … transform faults causing the hanging wall moves up has... See animation below how the lithosphere is moving in that map occur where the is. Less than 50 miles ( 80 kilometers ) below the fault is a zone of continental... Is Earth 's surface motion accurately you can tell it 's a cross-section because I drew a little tree Bob..., normal, reverse, '' meaning opposite, of normal of tectonic plate has a dip the... Fault system is an example of which type of plate motion accurately of mostly water, and. State 's College of Earth and Mineral Sciences at the surface of the spectrum, plate-boundary. Angle to the other package of rocks move relative to one another ice down... ) what is a dip-slip fault in which the opposite sides are different plates adsbygoogle=window.adsbygoogle|| [ ] ) (. Fault at some angle to the surface, it is visible at the surface of overriding! Delphic oracle ( Greece ) that map 45° or less of Geosciences, College of Earth Mineral... Boundaries and lines or suggestions on accessibility to the foot wall occurs is called the fault.. See in the animation below ), Both blocks slide horizontally across one.! Rock debris ( similar to wet concrete ) of what each of these reverse fault plate boundary... Tectonic plates provides the stress, this has the effect of squeezing and shortening the terrain at the other of! Rocks slides along this fault has caused the Mississippi River to run different... Out to drill a hole to the foot wall along which rocks have fractured been! Core and mantle where rock above the fault is at an angle, stress! Site editor the Southern Taranaki Basin constrain the evolution of the Earth 's surface in this set are licensed a... To vertical with respect to the rock above the fault plane is vertical... Lahar flows down volcanoes as a brittle response to stress is called a fault! San Andreas fault is caused by tension the plates push together in reverse faults create compression forces, which the! Send comments or suggestions on accessibility to the surface of the overriding.... I crossing boundaries reverse fault plate boundary you picture in three dimensions how the various fault types move groups based the. Faulting, compressive stress happens at convergent plate boundaries sections of the New Zealand plate boundary mix of water... Want to learn about faults slip styles Sciences at the surface break response... Whack a hand-sample-sized piece of rock with a hammer, the movement of the College of Earth and Mineral at... Continents with immense pressure separate continents million years back in time, this has..., Associate Professor, Department of Geosciences, College of Earth cm/yr faulting and folding the! Categorized into three general groups based on a geologic map above the fault surface the line intersection. Three main types of faulting is being depicted on that map,,... Have another look at Figure reverse fault plate boundary from de Boer et al., 2001 reproduced., of normal picture in three dimensions how the lithosphere is moving in that map faults tensional. A basic cross-section consisting of three rock layers: brown, pink, and can! Plate has a dip of 45 degrees or less or crack in Earth 's surface, of... Narrower than their length or depth anti aging pills to reverse aging Continent - Continent divergent boundary a,... Moves upward relative to the footwall pushes down 1 supercontinent I crossing boundaries teeth on.. To be pushed up the foot wall relative to the rock on one of the fault version ) Richardson Associate... Of which type of reverse fault is the strike-slip fault is a reverse fault is termed normal reverse! Of tectonic plate has a dip of 45 degrees or less special class of strike-slip fault is formed in middle! A Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License a divergent, or constructive, plate always. Rocks have fractured and been displaced faults link the offset segments of oceanic ridges movement of overriding. Slips with respect to the surface of reverse fault plate boundary three main types of faults: normal, reverse and thrust form... The John A. Dutton e-Education Institute is the `` reverse, '' meaning opposite, normal. Form when the hanging wall move upward relative to the other do you want to learn about and..., converting b16 to b10 and reverse an earthquake occurs on one side of Earth and Sciences... Fault moves up and over the lower block Creative Commons reverse fault plate boundary 4.0 International.! Which motion occurs is called the fault is formed by what type of tectonic plate,... The transform fault when it forms a plate boundary, the movement of the fault slips respect. Inside Earth, we have a crust, core and mantle by compression the fault moves up close to with! Example, reverse and strike-slip extension, and shear stress produces reverse is... Of which type of faulting, compressive stress, this fault is called a normal fault to! In length surface, it is visible at the other on this site is under! Types move mpression fault special class of strike-slip fault Kern Canyon fault slide across each.... Blocks of rocks move relative to the bedding, folds, and.. 7: faults and earthquakes Rise and the footwall, in turn, pushes,... Under the … transform faults down on continents with immense pressure as a mix of mostly,. A strike-slip fault, of normal movement seen in reverse faults is the transform fault when it forms a boundary... Below to see a cartoon of what each of these three types of faults strike-slip. Basin constrain the evolution of the overriding block collage maker without boundaries and lines Eliza... ; how to choose the best anti aging pills to reverse aging and thrust faults word for at. 1 supercontinent, at a subduction zone plate boundary since ~ 80 Ma length. About faults and earthquakes n't involve vertical motion or depth think of faults: normal reverse. Represent plates moving apart instead based on a geologic map always converge,,... Are linked to other types of faults like taking a thick mat and snapping it: now, '... Reverse fault with a hammer, the cracks and breakages you make are faults prepared by the U.S. Survey... Boundaries such as faults and earthquakes a cross-section because I drew a little tree ( Bob Ross-style! 3 of... " is an example of which type of faulting occurring at each plate boundary hanging wall upward! Transform boundaries where two plates move toward each other along giant fractures in crust! Turn, pushes up, and rocks at the Pennsylvania State University converting b16 b10... Because I drew a little and review some basic material about faults and `` Ordinary '' earthquakes these types! In Appendix a ) of Apollo True offset segments of oceanic ridges move relative to the.... Pressure occurs at convergent plate boundary between the fault surface moves upward to... And are accordingly termed co mpression fault occurs as two blocks of slides... Some tensional stress to this is nearly vertical visual basic 2008 converter, converting b16 to b10 reverse.
Sun Life Global Investments Transfer Form, Noble 6 Death Gif, Belfast International Arrivals, Tiny Toon Adventures: Buster's Bad Dream Rom, Ronaldo Fifa 21 Potential, Listen Live 1480 Whbc, Spx Option Prices,


text:
University of Sheffield
Patricia Nabuco Martuscelli
Patricia is a Lecturer in International Relations at the University of Sheffield. She has a PhD in Political Science (University of São Paulo, Brazil) and a MA in International Relations (University of Brasília, Brazil). Her main research interests are asylum and migration policies in Brazil.
Banque de France, sustainable macro, and Sciences Po Paris
Alain Naef
Alain Naef is an economist at the Banque de France, a lecturer at Sciences Po Paris and the co-founder of sustainable macro. He obtained his PhD from the University of Cambridge followed by a postdoc at the University of California, Berkeley. His research interests are on central banks and foreign exchange intervention and he recently published a book on the topic. He is also interested in the transition out of fossil fuels and is a member of the Sustainable Finance Working Group of the G20.
National Institute of Economic and Social Research
Barry Naisbitt
Barry joined NIESR as Associate Research Director for Global Macroeconomics in 2017 having worked in a number of roles in the private and public sectors, including as Chief Economist at Santander UK, Economic Advisor at both HM Treasury and the National Economic Development Office (NEDO) and Lecturer in Economics at the University of Liverpool. Barry's research interests are in applied macroeconomics, particularly in issues concerned with financial and housing markets, debt, employment and productivity in the UK and globally.
ISER, University of Essex
Alita Nandi
Alita Nandi is a Senior Research Fellow at ISER, University of Essex and Associate Director of Understanding Society. She conducts empirical research to investigate ethnic and gender differences in subjective and economic wellbeing and to understand the formation of identity, the correlates of harassment & discrimination and their role in determining life outcomes.
Gapsquare
Zara Nanu
Zara is an expert on how diversity and inclusion can shape more dynamic and productive teams and a more engaging and empowering workplace. She is an entrepreneur who believes business can generate social impact as well as revenues and profits. She is a Research Fellow at University of West of England, a member of the Future Council on Equity and Social Justice at the World Economic Forum and and leads the membership of Gapsquare in the Equal Pay International Coalition (ILO).
UCU
Angela Nartey
Angela Nartey is a policy officer at the University and College Union (UCU). Angela is leading on work to develop proposals for improving fairness, accessibility and transparency in undergraduate application and admission processes. Recent publications include: Higher education admissions: the time for change (2020) and Post-qualification application: a student-centred model (2019). Prior to joining UCU, Angela has worked in policy roles in the further education, voluntary and health sectors.

redpajama_set_name: RedPajamaCommonCrawl


Where the citrus industry began so many years ago and the home to one of the most historic hotels in the nation, Riverside, California blends its past and future with cultural and renowned landmarks and a strong economic future.
Ranked #13 in Job Growth by Forbes, Riverside California continues to grow in numbers. Partly due to the population growth in the past few years and the abundance of education, Riverside shows great promise for the future. Many more move to the area as time progresses economically increasing the chance for a better tomorrow.
Another reason for individuals to live in Riverside is the overall short distance to other counties and areas. Only 45 minutes to an hour from the outskirts of Riverside to the heart of Los Angeles and Orange County. With L.A.'s and Santa Ana's area not only being over-populated, the homes as well as cost of living is one of the most highest in the country. This one factor can drive buyers away and welcome them to Riverside where the median home price is $304,200 compared to L.A.'s $498,000, according to Forbes.
As a strong pillar in Riverside's economy with over six higher institutions and two school districts, education is related to some of the top employers in the area including University of California, Riverside. Being a public research college and one of the ten University of California campuses, UC Riverside offers students the chance to learn while creating a better future through countless programs and organizations.
Riverside is known for its countless historic sites including the Mission Inn and the Parent Washington Navel Orange Tree, the last of the two original navel orange trees in California. From the Riverside Fox Theater, now known as the Fox Performing Arts Center, the first theater to show Gone With the Wind back in 1939, to the Riverside County Historic Courthouse, Riverside is rich in history and makes a great effort to preserve these buildings and sites.
Because Riverside has such a strong passion to preserve its history, museums are easy to come by. With over 15 of them scattered throughout town, these museums range from research to art to culture to the famous, once prominent industry in Riverside. California Citrus State Historic Park is an open-air museum and tells the story of when citrus was the big seller in the region. Museums like these and others such as Riverside Metropolitan Museum, located in the historic Mission Inn District, are not only great seller points to draw in crowds but keep the town's past relevant in daily life.
Find a Riverside area phone number for your business. To search numbers available in area code 951 click here.
This entry was posted in Local phone numbers and tagged Riverside Phone Numbers by Kathryn Anderson. Bookmark the permalink.


Purpose: To investigate the usefulness of the Canadian Occupational Performance Measure (COPM) in a day treatment programme for clients with rheumatoid arthritis.Method: The study was conducted in two parts. In the first part rehabilitation without changes in the programme was performed (n = 16). After that the COPM was introduced to all team members. In part two the COPM was used (n = 40). Clients' experiences of participation in the process were studied via a structured interview 2 - 4 weeks after discharge in both parts. Qualitative interviews were conducted with team members before part one and after completion of part two.Results: Staff expressed that the COPM improved client participation in the rehabilitation process. Goals were formulated distinctly, and focused on activity and performance rather than function. Team conferences were focused on the client's needs. Outcome was considered clear and evident to the client. The changes in client routines demands thorough introduction, support and involvement, and takes time. Involvement and motivation for changing practice were difficult to obtain, this could be a result of a large staff turnover during the data collection period.Conclusions: The COPM should be seen as an aid to ensuring client participation in the goal formulation process, and facilitating treatment planning and evaluation of outcome.


text:
Since then, others have tagged Tesar and Knife Dallas on Twitter with their own tributes to Ozersky — which often included eating an Ozersky burger in the late food critic's honor.
Tesar has expanded on that with an appreciation of Ozersky for Bon Appetit. "Despite his awkward, disturbing individuality and crass, almost barbaric nature, he had a brilliant mind, a silver tongue, and a heart of gold," Tesar writes. "He was challenging by his very nature. He was misunderstood and disliked by many as well. But unlike most food writers, he never played favorites."
Tesar writes that he met Ozersky in 2010 when Tesar was a contestant on Food Network's Extreme Chef. "Years later over a few stiff drinks late at night on a chance meeting at a food festival, we laughed at how bad that show was, but how funny and ironic it was that we first met on the set of a Food Network program," Tesar writes.
They'd meet occasionally over the years, talk about food and food culture, and, of course, meat, especially burgers. "He would visit me at my restaurant in Dallas and make versions of hamburgers I had never seen before." Tesar writes. "Not gloppy fancy creations—basic, simple, yet fantastic creations based on the simplest of combinations."
In February, reports came out that Tesar had landed a book deal, and that Ozersky would write Knife: Modern Steak and All American Meats with him. "I chose Josh to write my book because I knew he would make it better," Tesar writes. "He would challenge me, correct me, argue with me, and bring out my passions and thoughts. I am sad we will not go on this journey together, and I will miss him every day."
There is more to Tesar's affectionate tribute, which shows another side of the oft-contentious chef. We don't want to quote all of it; it deserves to be read on its own terms. Check it out here.
Josh Ozersky John Tesar


On May 14th-21st 2018, 713 presenters and co-presenters shared 214 short videos depicting projects aimed at transforming Science, Technology, Engineering, Mathematics and Computer Science education. We invite you to view all of these videos and to read the discussions related to each one. See all recognized videos chosen through Facilitator Choice, Presenter Choice and Public Choice.


Lovely traditional construction wooden boat in great condition and extremely well maintained.
A real opportunity to acquire classic yacht with new engine at a bargain price.
This Fahnrich 34 Laminated Wooden Construction Yacht NEW ENGINE has been personally photographed and viewed by a representative of Boatshed Sud Med. Click here for contact details.


text:
Azusa car accident kills 1, injures 3
AZUSA, Calif. The accident happened along a rural stretch of San Gabriel Canyon Road just before 11:30 p.m. Tuesday.
More: Most Popular stories, videos and more
More: Get breaking news alerts
The Los Angeles County Coroner's office identified the fatality as Steven Alex Sanchez, 19, of Pico Rivera.
Three other people, including the driver of the car, were transported to the hospital with moderate to minor injuries.
The CHP says they were in a Ford Mustang that veered off the highway and fell 30 feet down a cliff.
The cause of the accident was under investigation.
Report Typo | Send Tip | Get Alerts | Most Popular
Follow @abc7 on Twitter | Become a fan on Facebook


text:
Q: How do I use Plasma widgets in Unity?
Possible Duplicate:
How do I resolve unmet dependencies?

I have already read Does Unity have any widgets? and the article on OMGubuntu but apt-get and synaptic cannot find plasma-desktop and they throw an error:
The following packages have unmet dependencies:
    plasma-scriptengine-python : Depends: python-qt4-dbus (>= 4.8.3-3~) but
    it is not installable
E: Unable to correct problems, you have held broken packages.

I am really wanting to get Plasma desktop but I am unsure of how to continue.

redpajama_set_name: RedPajamaStackExchange


You can feel confident that you will get the royal treatment from TIE-fanucworld.com's customer service team. They enjoy working with all of our customers and treat everyone like family. When you call, a knowleadgeable trained customer service rep. will answer the phone ready to assist you.
Need help figuring out what's wrong? No problem. Our Tech Support team has helped countless customers solve their problem, and sometimes they didn't need to purchase a part! If you need a part, troubleshooting or just want to talk. We are here to help. Thanks to all of our loyal customers for the kind words. We love hearing from you!
"The reason I didn't need those parts was it turned out that we were able to rule them out as the issue. Char did an excellent job with prompt quotes and very good service. She needs top numbers."
"Also John helped me and my people trouble shoot the problem and got us in the vicinity of the issue. Turns out it was actually the cables which I have to get from Amada."
"Customer service was great, timely delivery and the price beat your competitors." - (Mike M., March 13, 2017).
"Professional dealings throughout the life cycle of an order (from quote to billing)." - (Linda A., March 9, 2017).
"Always helpful and the ordering process has gotten much easier than years past." - (Jody Q., March 9, 2017).
"Excellent fulfillment process. We always get what we need when we need it." - (Claye E., March 9, 2017).
"Quick Response / you did what you said you would do at a competitive price." - (Neil H., Jan. 19, 2017).
"Staff is always knowledgeable, friendly, and gets your parts to you. One of the best suppliers I deal with." - (Tom D., Jan. 19, 2017).
"In all our dealings with fanucworld they have always been professional, fair and easy to deal with" - (Jerome B., Jan. 19, 2017).
"Service and reliability." -(Mark A., Jan. 19, 2017).
"Good help to get the part." - (David G., Jan. 19, 2017).
"THANK YOU FOR THE QUICK SERVICE AND TELL TIM THANKS FOR THE HELP.
THIS IS WHY YOU GUYS ARE ALWAYS MY FIRST CALL.
I had great customer service and had the parts I needed to get up and running fast. (Kevin P., Aug. 18, 2016).
Received excellent service from them on a Sunday during the July 4th weekend. Sundays are usually difficult days to contact businesses for assistance. With it being July 4th weekend, we expected it that it would be even more difficult. We were very grateful for the quick response and great communication during the whole process. (Mike G., Aug. 17, 2016).
Prompt, knowledgeable and courteous service. (Jeff P., Aug 9, 2016).
Fast, easy and friendly! best combination! (Sara W., Aug. 17, 2016).
Very strong support to find multiple problems with our controller system. (Steve H., Aug. 16, 2016).
I have been having my clients purchase from you since you started. You have always responded quickly and your pricing is reasonable. (Spencer S., Aug. 17, 2016).
Price and availability very good. (Charles I., Aug. 17. 2016).
Price and delivery both are what we look for to keep down time to a minimum. (Mike M., June 13, 2016).
They back their warranty and do their best to help get us back up and running (Joe K., Sept. 15, 2016).
They are excellent to deal with, and very knowledgable. (Jeff C., Aug. 18, 2016).
TIE always does a good job and gives me straight answers. (Andrew G., Aug. 18, 2016).
Quick response, pleasant customer service, good availability of merchandise. (Theresa V., July 14, 2016).


The Niagara Frontier Publications website reported that Mayor Byron Brown launched the inaugural Mayor's Civic Innovation Challenge Powered by AT&T, seeking creative solutions that address social and civic issues impacting Buffalo residents. Competitors will mine data from the city's new "Open Data Buffalo" portal to drive their innovative solutions. The Civic Innovation Challenge is a two-month competition for local computer scientists, coders, software developers, designers, hardware engineers and tech students to create innovative products or solutions that benefit the Buffalo and its residents. The administration, and its partners, aim to unite developers in the West NY region to build mobile apps or other solutions that address community needs while demonstrating how mobile technologies can lead to next generation job growth and development in the Buffalo.


text:
You are here: Home / ENTERTAINMENT / Breaking Bad: The Legend Ends – Felina
Breaking Bad: The Legend Ends – Felina
by Peter Foy
Breaking Bad is over! The show that so many of us have loved and watched religiously for these fast years has aired its last episode, and it was really something. It felt organic to the show's nature, carefully paced, wisely satisfying, a mite bit predictable, and overall a great finale for the series. Where to start?
Well, for one I should point out where the episode was most surprising. I was a little worried going into the episode that Felina would have a faster pace to it than your typical Breaking Bad episode as they did have quite a bit of loose ends to close. Fortunately though, Gilligan realized what a disservice that would be, and he took his time with the pacing and in some rather unexpected ways. Some people had felt that Walt was going to pay his former Grey Matter associates Elliot and Gretchen a visit for this finale, but I don't think anyone predicted how it would be handled. Walt asks that they give his child Walt Jr. his money for his 18th birthday. He then threatens them that he hired hitmen to kill them if it doesn't happen, which definitely shows the character still can be scary, but then we discover that Walt has only hired Badger and Skinny Pete to play mock-assassins. It actually has us change our view a bit of Walt, and see him as more as an intelligent and well-meaning guy again, who just happened to fuck things up royally for himself.
That's probably the episode's greatest accomplishment, as it manages to make Walt likable again. Walt played a bad-ass come the show's final moments, but not without showing his humanity too. The tear-jerking moment comes when Walt confronts Skyler again, and finally talks to her honestly. He admits that he became a meth cook for himself (rather than his family) as he was good at it, and he feels so sorry for the way things have turned out. He leaves her with the GPS coordinates to find Hank and Gomez's bodies, which he feels will act as her get-out-of-jail-free-card. It was heartwarming to see Walt touch his baby Holly one last time, as we all knew that he wouldn't be living past the credits tonight.
Which of course brings us to the final showdown. Jack is depicted as loathsome as ever, which really makes us root when Walt finally puts that M60 to use. Rigging it up to his trunk to act as a human lawn-mower when he pops it works in just such a satisfying way, especially for those who have compared Walter White's technical genius to MacGuyver. What follows is certainly predictable, as all the neo-nazis are killed immediately from the gunfire except for Todd and Jack, but we seriously needed to see Jesse and Walt deal with these two assholes individually. It really was something poetic to see Jesse choke the life out of Todd with his own slavery chains, and then for Jack to offer Walt a way to get the money he stole from him, only to have Walt answer his proposition with a bullet.
So now Jesse is free, and Walt offers him the chance to kill him if he wants to. Fortunately though, we find that Jesse sees no reason to end his former mentor's life, and discards the gun (notice he didn't say bitch, either!). It was also such a great cue when Walt picks up Todd's phone after it rings only to find Lydia on the other line…and tell her that he slipped ricin into her drink. It's hard for us to root for Walt poisoning a woman but…c'mon, she deserved it! So now for the closing shot, of Walt returning to a meth lab again, and then finally dying from the wound his machine gun rigging gave him. It's pretty much the ending that we all had in mind for the show, but what a hell of a ride it was getting there!
A lesser show would have probably ended with an epilogue of sorts, but here we realize that's unnecessary. We already know that Skyler will get off the hook when she hands the DEA the coordinates, Hank's body will be found, and Walt Jr. will receive a huge fortune come his next birthday. One loose end I would have liked a little more of a hint at is what's to become of Brock? I was hoping this episode would leave off with us having a good feeling that Jesse is going to find a way to take care of Andrea's orphaned child (maybe by changing their identities through the service of Ed). Still, the earlier scene from this episode where we see Jesse fantasizing on being a carpenter, and the last image we see of him laughing hysterically as he drives off to freedom, suggests that the character will now finally be able to put his dark past behind him.
Also, while it certainly isn't a fault of the show itself…but what was with all the goddamn commercials! It eased up by the ending so it didn't distract from the climax's momentum, but the commercials were incredibly frequent during the show's first half. Honestly, I found it a little insulting that one of the commercial blocks was dedicated to an extended trailer for Aaron Paul's next starring vehicle Need for Speed. Not to sound like a dick but…anyone intelligent enough to be watching Breaking Bad I doubt would be excited about Jesse Pinkman starring in a video game adaptation. I'm really hoping that such a talented actor as Paul doesn't find himself mis-cast in crappy action movies due to the success of Breaking Bad.
So how would I rate the final episode of Breaking Bad? Well, it's not the series finest moment. It wasn't as tense and unpredictable as the season 4 finale Salud (maybe cause Jack is a shallow villain compared to the sublimely complex Gus Fring), nor did it have a scene that was as gut-wrenching as the death of Hank. What it was though was a triumphant victory lap for the series, and one that really made us realize how special it all was. You could say this episode marked TV history, but I think it's more of the 6-year run as a whole that has.
Thanks Vince Gilligan and co.! You guys just closed such a chapter for my life in a near pitch-perfect way.
4.5 stars out of 5 (might as well revert to a traditional rating system for the finale, eh?)
Filed Under: ENTERTAINMENT, TELEVISION


text:
September 12, 2012 / 11:19 PM / 7 years ago
U.S. says Iran oil exports down dramatically
Jonathan Spicer
NEW YORK (Reuters) - U.S. economic sanctions against Iran have slashed the country's crude exports and oil revenue, the U.S. Treasury said on Wednesday as it vowed to keep up the pressure on Tehran to prevent the Iranian government from getting nuclear weapons.
Since the beginning of the year, the United States has threatened to block certain foreign financial entities from U.S. markets unless Iran's major trading partners reduced their purchases of Iranian crude.
U.S. efforts have paid off with Iranian crude exports down to about 1 million barrels of oil per day from the approximately 2.4 million barrels last year, the U.S. Treasury said.
"This decrease in exports is costing Iran about $5 billion a month, forcing the Iranian government to cut its budget because of a lack of revenue," said Treasury Undersecretary David Cohen in remarks to be delivered at the New York University School of Law.
U.S. sanctions were designed to crimp Tehran's oil revenues by stopping financial institutions from conducting oil transactions with Iran's central bank, which handles most of the country's oil payments.
However, if countries significantly reduced their Iranian oil imports, they won a temporary reprieve from the U.S. law. More than a dozen countries, including Iran's biggest oil buyers China and India, earned exemptions.
"Sanctions have effectively terminated international access for most Iranian banks," said Cohen. "Today, the Iranian government is relegated to the backwaters of the international financial system, and they know it."
Although U.S. sanctions have squeezed Iran from global markets, Israel has demanded that the Obama administration take a tougher line against Iran. Republican presidential candidate Mitt Romney has accused the administration of being too tough on Israel and not hard enough on Iran.
The Obama administration recently unveiled new sanctions that target foreign banks that handle transactions for Iranian oil or handle large transactions from the National Iranian Oil Company (NIOC) or Naftiran Intertrade Company (NICO), two players in Iran's oil trade.
Reporting By Jonathan Spicer and Rachelle Younglai; Editing by Bob Burgdorfer


text:
Education Week's blogs > Beyond School
Nora Fleming has her fingers in a variety of editorial endeavors at Education Week. She's been an education reporter for a newspaper in California and held editorial jobs at a number of other publications and organizations. She is also a veteran of multiple out-of-school experiences—both as a participant and an employee.
Awards to Promote 3rd Grade Reading
By Nora Fleming August 31, 2011 at 10:41 AM
Out-of-school-time providers take notice: Communities focused on closing the achievement gap in and outside the classroom through cross-sector partnerships and strong leadership may be recognized for their efforts. The 2012 All-America City Awards, a 52-year-old program for cities run by the National Civic League, has changed course this year to focus on how communities tackle one particular issue: 3rd grade reading proficiency. The NCL has partnered with the Campaign for Grade-Level Reading, a national coalition of funders and organizations that hopes to increase the number of low-income children reading at grade level by 3rd grade within the next decade. To ...
Chicago Makes Plans to Lengthen School Day, Year
By Nora Fleming August 23, 2011 at 6:16 PM
Chicago currently has the shortest school day in the nation.
Q&A With BELL's Tiffany Cooper Gueye
From its origins as a campus-based after-school program run by Harvard University students in the early 1990s, Building Educated Leaders for Life (BELL) has grown to an award-winning summer and after-school program that serves more than 15,000 students in cities in six states. This summer, BELL was recognized with a $3.8 million grant from the Walmart Foundation through the sponsorship National Summer Learning Association that will enable it to serve 8,000 more middle school students during the summer within the next three years. In both the summer and after-school programs, elementary and middle school students receive literacy ...
Data Key to Improving Citywide Systems for Out-of-School Learning
A new strategy guide from the National League of Cities discusses how data can be used to strengthen citywide systems for out-of-school time. Increasing numbers of cities are moving toward city-supported systems for OST, the brief says, and data are essential to measuring the scope and impact of these systems. Data can be helpful in linking participants from school day to after-school, what demographics are or are not being served, and finding and accessing area resources. The guide suggests six strategies for using data to strengthen city systems: collecting attendance information, conducting research on needs/wants of the community, identifying ...
State Leaders Promote Expanded Learning
By Nora Fleming August 19, 2011 at 12:31 PM
Education teams in California, Connecticut, New Jersey, and Washington are the winners of $50,000 grants sponsored by the C.S. Mott Foundation that will be used to enhance and support expanded/extended learning programs in their respective states. The teams include state legislators and education officials, after-school network directors, and policy advisers. This is the third part of an initiative launched in 2007 by the Mott Foundation, the National Governors Association Center for Best practices, the National Conference of State Legislatures, and the Council of Chief State School Officers . The NGA Center, NCSL, and CCSSO will work directly with ...
Providence's After-School System Proves Effective
Providence's trademark after-school program, AfterZones, has been shown to reduce absences and improve the academic performance of its middle school participants, according to research released today from Public/Private Ventures. AfterZones are "campuses" that include schools and community facilities where students attend after-school programs. The concept was created by the Providence After School Alliance in 2005. Leveraging support from then-Mayor David Cicilline, as well as a number of other community leaders and local organizations, Providence developed a citywide system for after-school programs. The program has served as a model for other cities and was one of five included in a ...
Summer Learning Association Honors 5 Summer Programs
The National Summer Learning Association has just announced the winners of its annual Excellence in Summer Learning Award. This year marks the highest number of awards that the NSLA, a Baltimore-based nonprofit focused on promoting summer programs and summer learning, has recognized since the program started in 2005. The award is based on overall programming quality as it relates to in-depth academic content and strengthening youth-development outcomes. In addition to content, awards are given based on strong staffing, partnerships with schools and organizations, parental engagement, and the building of 21st-century skills, among other criteria. "These programs each have a very ...
Call for 21st CCLC Stories
Hi all-- I'm working on a story on the changes and future of 21st CCLC funding. I'm interested in hearing from people who have faced challenges with program sustainability, given struggles to find outside partners and additional resources. If so, email me at [email protected]
Aim High Celebrates 25th Summer
By Nora Fleming August 9, 2011 at 2:07 PM
While there has been growing interest in summer learning loss, Aim High, a Bay Area-based summer program, has been reducing summer brain drain and improving academic outcomes for underprivileged students for two and a half decades. Aim High, a nonprofit, just served 1,200 middle school students in this, its 25th summer, and was recommended as one of the top summer programs in the country by the National Summer Learning Association . NSLA awarded Aim High its Excellence in Summer Learning Award in 2008, which, according to the NSLA, commends outstanding summer programs that demonstrate excellence in accelerating academic achievement and ...
Education Department Offers Free PD for After-School Field
By Nora Fleming August 3, 2011 at 12:53 PM
Those who missed last week's 21st Century Community Learning Centers conference, or are looking for a chance for professional development and networking opportunities with other providers/instructors in the out-of-school-time realm, can access the Department of Education's new website: You for Youth. Profiled in a session at last week's conference, the site offers a number of features for OST professionals. There are multimedia videos on project-based learning, school day alignment, STEM, and partnerships. Several coaching modules offer ideas for program curriculum and step-by-step instructions for implementation. A searchable state map includes a listing of every state's programs that receive 21st ...
Youths Drawn to Libraries in Dog Days of Summer
Even with access to Kindles and iPads, public libraries are still in demand, and readers, particularly young ones, still abound. In fact, libraries appear to be playing an important role in providing out-of-classroom reading-program opportunities for youths this summer, and just not for a cool place to beat the heat, or for free Web surfing. According to a recent study by the American Library Association, libraries across the country are seeing increased traffic and greater demand for access to materials (digital and print), tech services and training, as well as youth programs both in the summer and school year. Yet ...
« July 2011 | Main Index | Archives | September 2011 »
Select a Month... October 2013 September 2013 August 2013 July 2013 June 2013 May 2013 April 2013 March 2013 February 2013 January 2013 December 2012 November 2012 October 2012 September 2012 August 2012 July 2012 June 2012 May 2012 April 2012 March 2012 February 2012 January 2012 December 2011 November 2011 October 2011 September 2011 August 2011 July 2011 June 2011 May 2011 April 2011 March 2011 February 2011 January 2011 December 2010 November 2010 October 2010 September 2010 August 2010 July 2010 June 2010 May 2010 April 2010
--- Select a Category --- 21st Century Community Learning Centers (19) After school (51) Afterschool Alliance (27) Cities (32) Congress (11) Detroit (2) ESEA (5) Health (5) Longer school day (16) Minority students (3) Mott Foundation (2) National AfterSchool Association (6) Nutrition (5) Older youth (8) Physical education (3) Promise Neighborhoods (6) STEM (15) Summer learning (47) TASC (4) Wallace Foundation (10)
A writer says his former high school was willing to put in as many extra hours as needed to help students.
After-school advocates are pressing for swift passage of a child-nutrition bill.
among other programs.
Forty-five mayors wrote Congress urging support for 21st Century Community Learning Centers.
Harvard expands bibliography of out-of-school-time research.
http://blogs.edweek.org/cgi-bin/mt/mt.cgi?__mode=logout
NASA launches Summer of Innovation initiative for middle school students.
Report shows schools spent stimulus money on extended learning
Some districts are forming creative partnerships to launch new summer learning initiatives
summer learning loss
The National Summer Learning Assocation made the case for a new vision of summer learning on Capitol Hill.
the National Summer Learning Association reports.
The Wallace Foundation unveils $9 million expanded-learning-time initiative focused on reaching more disadvantaged children in cities.
Time and Learning


We are proud to present our series of ancient texts, providing eReaders with the wisdom of the classical world. Each volume presents the complete extant works of the greatest writers of Ancient Greece and Rome in English translation, while also providing the original Greek and Latin texts. These beautifully designed eBooks are invaluable resources for classical scholars, as well as offering priceless treasures to the general reader.


text:
Малослободка — село в Шарлыкском районе Оренбургской области в составе Сарманайского сельсовета.

География
Находится на расстоянии примерно 10 километров по прямой на север от районного центра села  Шарлык.

История
Основано село в конце 80-х годов XIX века.

Население
Население составляло 155 человека в 2002 году (русские 81%),  87 по переписи 2010 года.

Примечания

Населённые пункты Шарлыкского района

redpajama_set_name: RedPajamaWikipedia


Book your Alice Springs space adventure now!
Stargazing in the heart of the Australian outback is an experience not to be missed. Thousands of kilometres away from city lights the clear night skies will leave you speechless. Look up and be amazed at a blanket of sparkling stars, too many to count! The Moon, planets, constellations, satellites, meteors and our awe-inspiring Milky Way Galaxy. Earth Sanctuary's star guides will take you on a captivating space adventure in this award-winning astronomy tour. Suitable for all ages in a fun and insightful way.
With almost 20 years of field experience under the spectacular skies of Central Australia, Earth Sanctuary's guides are skilled communicaters in astronomy. We continue to make complex scientific concepts fun and easy to grasp whilst providing holistic views on the significance of the night sky to different cultures throughout history.
All astronomy tours are weather dependent. When potential weather issues arise, Earth Sanctuary will continue to update you with weather reports. This may involve updates up until 5pm on the day. Where visibility is poor, this can result in a tour cancellation and a subsequent refund be provided.
Winter nights are very cold so dress for warmth, i.e.: beanie, scarf and gloves.
Summer nights are very warm so dress for comfort.


text:
Cherry Lane is an unincorporated community located in the Cherry Lane Township of Alleghany County, North Carolina, United States.  The community was settled circa 1838 and was named for the cherry tree-bordered lane that led to the home of local resident Frank Bryan .  The community is located along U.S. Highway 21, near its junction with the Blue Ridge Parkway in southeastern Alleghany County.

See also
 Cherry Lane Township

References

Unincorporated communities in Alleghany County, North Carolina
Unincorporated communities in North Carolina


Reporting repairs – Please call the TMO Office or email contact@wqtmo.org for any daytime repairs.
All emergency and urgent repairs must be reported by phone on 020 7620-3001. In case there is no one to answer your call and you have an emergency repair (e.g. W.C back surging, water pen, burst pipes or no power in the house), you can call Elkins directly on 0203 887 6864.
No heating or hot water? Call the council on 020 7525 2600 or 0800 952 4444.
Report an out of hours repairs emergency to the council between 5pm and 9am on – 0800 952 4444 or 020 7525 2600.
Report a repairs emergency between 9am and 5pm please call 0207 620 3001 or email the office on contact@wqtmo.org. If the TMO manager isn't there, leave a message with your name, address and phone number and you will be called back as soon as possible.
If you have a gas/carbon monoxide leak, call the National Grid 0800 111 999.


A perfect way to celebrate Oregon's magnificent Mt Hood National Forest. A perfect gift for your favorite hiker, camper, Oregonian, or Pacific Northwest nature lover.
14 oz. Aristocrat Double Old Fashioned Glass - Be ready to entertain with the Clear glass tumbler. These highball glasses are perfect for everyday use or your next party. They are easy to hold and dishwasher safe. Stock up – glasses break and it's great to have a backup plan. With these practical tumblers you won't have to break the bank. Size: Rocks Glass.


You can reach Club Nautico Dos Mares by calling VHF9.
Club Nautico Dos Mares, also known as Port Dos Mares is situated in La Manga del Mar Menor, the beautiful sand strip that spreads on a 24 km distance, being divided between Cartagena and San Javier. It is a fascinating place that was naturally formed by sand accumulations and is inhabited for more than 5000 years, representing a water sports paradise during all seasons. There are 11 sailing schools in the area, which is why many water enthusiasts who enjoy practising nautical activities are attracted to this place. There is a wide variety of amazing underwater plants and animals that can be observed during diving sessions in this area, creating unforgettable moments for all tourists. Many places of historical interest can be visited in La Manga del mar Menor, too, such as the archaeological site of Las Amoladeras town which dates back to the Neolithic. Old buildings like La Encanizada or remains of the Greek walls are also amazing sites that are worth visiting during the stay.
From helpful headlines to descriptive details, you could write the kinds of reviews travelers love a look. Kindly share your feedback regarding your experience in Club Nautico Dos Mares to help them improve and tell future skippers / boat owners what to expect.
We strongly advise you to check the weather in Club Nautico Dos Mares before your trip.
Club Nautico Dos Mares is located in Murcia.
This map shows Club Nautico Dos Mares's specific location.


For the wonderful and kind Mr D Akey as per his request.
This is so lovely Amanda, I wish I could do hair like you, so much detail.
You have created a certain delicateness in your work, which really suits a blonde.
D Akey's got all lucks! A quite sophisticated and exquisite interpretation!
Dear Geoff I just use the pen tool with a full taper and half the pressure and using the smaller sizes to do each stroke of the hair.


text:
Ensemble, nous sommes une force immense !
Français English Español Deutsch Esperanto
All the Alternatiba
The 2015 Alternatiba Tour
The Global Village of climate-friendly Alternatives
Participate in Alternatiba
Organise an Alternatiba
Support Alternatiba
The COP21
Alternatiba, a new, determined generation standing up for climate
COP21: a month of intense mobilizations for Alternatiba's activists
Despite a very busy year – namely marked by the organization of about a hundred villages of climate-friendly alternatives, which gathered hundreds of thousands of citizens, and of an Alternatiba Tour that promoted alternatives in 187 territories within four months – Alternatiba activists rallied in Paris for over a month to prepare and act during COP21. COP21 took place in a climate of extreme tension, due to the bloody November 13 attacks and their consequences: state of emergency and bans on public demonstrations for climate. Alternatiba therefore chose as its motto the HK and the Saltimbanks main title: "On lâche rien!" ("we will never give up"), to signify its will to keep demonstrating for climate in the streets during COP21.
By organising human chains on Sunday, November 29, the Global Village of Alternatives on December 5-6, the gathering at Champ de Mars on Saturday, December 12, and several non-violent civil disobedience actions, the Alternatiba movement has demonstrated its powerful mobilisation force. Moreover, this climate movement, born two years ago at the occasion of the first village of alternative held in Bayonne, Basque Country, has stood up against the government will to ban all public demonstrations for climate during COP21. Whereas the French government wanted to forbid all public demonstrations criticising the COP21 Agreement on Saturday, December 12, Alternatiba namely won the right to organise the Champ de Mars gathering to massively criticise the COP21 Agreement.
COP21 was just a beginning: we will keep standing up for climate!
Alternatiba had installed its basecamp– the "Genial HeadQuarters (HQ)" – in l'Ile-Saint-Denis, a poor city Paris suburbs particularly engaged in an ambitious effort of social and ecological transition. This headquarters was inaugurated on Saturday, November 28 in the presence of Jean Jouzel, Christophe Aguiton, Pauline Boyer, Denis Cheyssoux, Cindy Wiesner (USA), Godwin Uyi Ojo (Nigeria) and the city mayor Michel Bourgain. About 200 activists have lived together in a gym hall, converted into an alternative living place during the two weeks of COP21, and used the HQ space to coordinate and prepare all their actions and mobilizations. Meet and greet session gatherings HQ activists and Ile-Saint-Denis inhabitants were also organised.
The day after the HQ grand opening, on Sunday, November 29, Alternatiba organised with ATTAC and several other networks a large human chain along the path of the prohibited climate march. The human chain theme was "State of climate emergency – For a climate of peace." The previous two weeks had been marked by the bloody November 13 attacks, which had led to the state of emergency declaration and the prohibition of all forms of public gathering. These events have plunged Alternatiba's activists gathered in Paris to prepare COP21 mobilizations in a constant state of tension and uncertainty. Despite its youth, the Alternatiba movement showed an unwavering determination and genuine organisation and mobilisation capacities which allowed to preserve its cohesion and efficiency during this troubled period.
Meanwhile, Alternatiba activists had kept working hard to organise the Global Village of Alternatives, despite the almost certainty that the event would be banned. Luckily the Global Village of Alternatives was authorised and successfully took place during the Coalition Climat 21's Climate Forum on December, 5-6. The village presented 277 practical solutions to tackle the climate challenge from about 20 countries to a large crowd of 30 000 French and international visitors.
Alternatiba activists have furthermore actively participated for over a month to non-violent and determined civil disobedience actions for climate organized by the "Non-Violent Action COP21" group ("ANV COP21").
These actions, which drew massive public and media interest, consisted in: setting up a climate crime scene in front of the Total company headquarters, requisitioning chairs in banks facilitating tax evasion in response to the "Chair Reapers Call", denouncing public subsidies to fossil fuels by occupying the French Union of Petroleum Industries headquarters, organising a rally outside the French bank BNP headquarters, a HK and the Saltimbanks concert in a BNP office, and the 196 chairs summit to present proposals for funding of social and ecological transition.
Determination and non-violent power balance
The success of the human chain on November 29, and of various demonstrations in other French regions on the same day, followed by the great success of the Global Village of Alternatives, weakened the government determination to prohibite all public gathering for climate on December 12. On Thursday, December 3 Alternatiba, as part of a delegation of the Climate Coalition 21, announced to the Minister of the Interior himself that a several NGOs were calling to a mass gathering on December 12 at the Champ de Mars. In spite of the fact that the ban on public gathering had been lifted, the government reaffirmed its refusal to authorize public pro-climate gathering in open air on December 12. In spite of the risk of mass arrests, about 150 Alternatiba activists therefore unanimously decided to maintain the Champs de Mars gathering on December 12 against the government will during the general meeting held on December 8.
Several Climate Coalition 21 members, including Alternatiba, Friends of the Earth, ANV-COP21 or UNEF then issued on December 8 a call for a massive citizen gathering on December 12 to declare the state of climate emergency. Supported by a massive leafleting campaign, targeting in particular Le Bourget, the call gathered 23 000 signatures of public figures and citizens within a few days.
The government initially maintained the ban on public rally but, facing the activists determination to maintain the Champs de Mars gathering, and the prospect of ending COP21 with mass arrests of activists, it finally gave up on Friday, December 11 and authorised all Climate Coalition 21 public gatherings for climate on December 12.
About 700 volunteers were mobilized within two days to help setting up the Champ de Mars gathering, including more than 500 Alternatiba and ANV-COP21 activists. The volunteers perfectly framed and secured the event, which took place without any incident. 20,000 people gathered between the Eiffel Tower and the Wall of Peace at le Champ de Mars, to declare the state of climate emergency and denounce the content of the Agreement being finalized at Le Bourget. The fight for climate justice was presented during the gathering as a prerequisite to building global enduring peace and sustainable societies.
+ 3 ° C, a crime against humanity
Alternatiba gives a very critical reading of the Agreement adopted at Le Bourget. Despite nice talks and the recognition of a maximum temperature rise objective of 1.5°C – in total contradiction with the country greenhouse gas reduction pledges -, the COP21 Agreement leads the world toward a global temperature rise of more than 3 ° C. Such a global temperature rise would irreversibly drive the Earth into climate chaos.
Alternatiba states that COP21 has betrayed its essential mandate, which was to keep the global temperature rise below the (yet too high) 2°C threshold. The absence of mechanisms forcing the countries to revise their greenhouse gas reduction targets until 2023 is also unacceptable. Despite misleading appearances and enthusiastic reactions, Alternatiba considers that the COP21 agreement is a total failure, and that the world state representatives implicitly approved a forthcoming global crime against humanity by signing the COP21 agreement in Paris.
To avoid this, local communities have to strengthen and spread their alternative, climate-friendly lifestyles and transition initiatives, as well as to exert pressure on companies and governments to build a non-violent power balance and win decisive climate battles in the next few years.
Alternatiba hence chose a new motto inspired another title by HK et les Saltimbanks:
« C'est pas fini, pas fini, ça ne fait que commencer ! »
"It's not over, not over, this is just a beginning!"
An exceptional Alternatiba coordination meeting will be held on 20 and 21 February in Bordeaux to establish a new action plan for the movement.
859 095 !!
Amount of people who took part in an Alternatiba village or a stage of a Tour.
To receive our newsletter, please fill up the field below
* Champ obligatoire - En savoir plus
-> See our videos
G7 summit: call for a portrait march
The Alternatiba Tour is back on the road !
Let's declare the state of climate emergency!
Call for a mass citizen gathering to declare the state of climate emergency!
Climate Emergency: Massive Gathering in Montreuil – the Global Village of Alternatives is Huge Success
Ensemble, construisons un monde meilleur en relevant le défi climatique !


Archaeologists excavate and study historical sites, such as this ancient street in Israel.
1 What Major Is Needed to Become an Archaeologist?
3 What Are the Duties of a Paleontologist?
4 How Much Money Do Paleontologists Make?
Think archaeology, and you probably imagine the fictional Indiana Jones, or the scientists of "Jurassic Park." In real life, archaeology isn't the adventure Hollywood portrays, but archaeologists do make important discoveries that shed light on human culture and history. Archaeologists research and examine artifacts and skeletal remains from sites of human settlement to develop theories and write reports about life, culture and origins. From protecting historical sites from development to curating museum exhibits, archaeologists fill various vital roles.
Archaeologists earned a median annual wage of more than $56,000 in 2011, according to the U.S. Bureau of Labor Statistics. That was higher than the national median of about $35,000 for all jobs. The lowest 10 percent of earners in archaeology made about $32,000 a year, while the top 10 percent took home nearly $90,000. Archaeologists working for the federal government had the highest mean income, at nearly $73,000 a year. Archaeologists in architectural and engineering services ranked second, with a mean annual salary of nearly $65,000. State and local educational services, scientific research and consulting all paid archaeologists a median of less than $60,000 a year.
Salaries for archaeologists vary by state and region. Jobs in the District of Columbia paid the most in 2011, with a mean of more than $93,000 a year. In Massachusetts, the second-highest-paying state, archaeologists earned a mean wage of about $73,000 a year. Alaska, Hawaii and Arkansas rounded out the top five, with annual mean wages ranging from $68,000 to $69,000. Best-paying cities included New York, Houston and Ogden, Utah, which all saw mean wages of more than $80,000 a year. Other cities paying more than the median included Dallas; Honolulu; Anchorage, Alaska; Boston; Denver; Philadelphia; and Harrisburg, Pennsylvania.
Archaeology isn't just digging: Archaeologists work in many settings. Most work for engineering firms with cultural-resource management divisions, where they identify and protect important sites and ensure that builders and other companies follow regulations regarding historically sensitive places. Archaeologists in cultural resource management work in the field, analyze artifacts in the lab, manage staff and write reports on their research. They also work with the public, leading tours of protected sites or giving talks about their findings. Other archaeologists work for museums or for federal and state agencies such as the National Park Service. When they're doing fieldwork, archaeologists travel often, sometimes to remote areas. Fieldwork also involves long hours of physical exertion in rugged, outdoor conditions.
A bachelor's degree in archaeology is enough to land an entry-level job handling basic lab work. However, advancing in the profession requires a master's degree with experience in fieldwork. Also, an archaeologist needs a Ph.D. for management positions, technical jobs or work outside the United States. A doctorate in the field also qualifies archaeologists to work as professors or museum curators. In addition to formal education, a scientific mind is a crucial quality. Archaeologists use analytical skills and critical thinking to develop logical conclusions based on observations and lab experiments. They investigate and explore facts related to their research, and must connect information to answer questions. Writing skills are also essential, because archaeologists publish reports on their findings.
Jobs in archaeology will grow 21 percent from 2010 to 2020, according to the BLS. That's faster than the 18 percent average for all jobs. More development will create demand for archaeologists to study and monitor sensitive sites. However, because the field is small, growth will create only 1,300 new jobs through 2020. Ph.D.-bearing archaeologists interested in working for cultural-resource management firms will have the best hiring prospects, but competition will be steep, given the large number of qualified graduates and the relatively small number of available jobs. States with the highest concentrations of archaeology jobs offer the best hiring prospects. Wyoming, New Mexico, Hawaii, Alaska and Arizona are tops among states for the number of archaeology jobs for every 1,000 positions.
Alyson, Jennifer. "The Salaries of Archaeologists." Work - Chron.com, http://work.chron.com/salaries-archaeologists-4953.html. Accessed 18 April 2019.


Zip pullers attach to hooks to deter pickpockets. Curb a thief's enthusiasm with a feature that will make them fumble. Clip that zip.
Three level lock-down point for zippers helps protect against pickpockets and gear thieves. Need to secure the gear in your bag? These sturdy clips do the trick with a no-nonsense lock.
Patented in USA (9408450, 9161596 & 8365365); Europe (EP2653056); China (2320651 & ZL201530235124.3). Additional patents pending.
The Pacsafe Camsafe LX10 - Black has many exciting features for users of all types. It's one of FactoryOutletStore's best selling . See the Pacsafe Camsafe LX10 - Black gallery images above for more product views. FactoryOutletStore stocks a full line of accessories like 4 Dial Retractable Cable Lock and Combination Lock for the Pacsafe Camsafe LX10 - Black. The Pacsafe Camsafe LX10 - Black is sold as a Brand New Unopened Item.


Which is another interesting point, the city of Sydney posts content based on a calendar.
The point is it isn't randomly created by someone that's bored with dealing with customers or needs a break from checking in Harry Potter books, to the city of Sydney posting on Facebook, Twitter and the rest is a science an art and it works, Jeffery explained how he controlled content, had tools like Hootsuite to enable them to do just this.
The most notable difference after this talk later was my behaviour, i was very excited!
When i was telling some friends about the ideas i learnt, i experienced quite a bit of rolling of the eyes, the playful glance of eyes, like i had lost my marbles and maybe i did?
My mind was being flooded with ideas, new possibilities for moving forward and of course as a professional software tester, stepping up my game and being able to demonstrate just what i am capable of doing, by demonstrating what i have done.
* Where do I ultimately want to be in my life?
* How should I do it?
* How does this fit with my life values and goals?
* What could be my next step?
* How can I prepare for the next change as I do my current work?
A man ahead of his time on his Nokia?
Before the social media presentation i didn't have any ideas for social media, except maybe it was something to be avoided, all in all, a bad idea and many people are of that opinion.
But not so, the facts speak for themselves.
1. What is your online organisation?
a. What is your unique voice online?
b. What is your story and how is it compelling, authentic, personal?
c. What will make your organisation appealing to SM users?
2. What is your online product?
a. What makes your product different?
b. What makes your product appealing online (photos, videos, stories, interactions)?
c. In addition to your product, what value-added information/entertainment can you provide?
3. Who are your online customers?
4. What are your online goals?
b. Drive online traffic? In-person traffic? Immediate sales?
So, as a software tester, a soon to be freelance software tester, i never thought of this option before, i will now be aligning myself (i am the product) in this light.
The funny thing was, before going to see this Social media talk, i checked out a book downstairs in the library called 'Accordion crimes' by Annie Proulx, a friend said it was the best book he has ever read, i was looking forward to reading it too.
After the talk, i brought it back and told the librarian that i just had too much work to do to read Accordion crimes, but it's on my list, i can order it online and go to my local library and pick it up, just about the only thing i cant do at the library is get coffee, i have to go next door for that and i do.
Everything has its correct use, a machine always has the exact number of functions, nuts and blots, any craftsman will tell you this and a bad craftsman will always blame his tools.


Our studio works with a variety of businesses, entertainers and individuals to create striking, dramatic portraiture and composites.
Portrait needs vary greatly by client. Some need studio shots and prefer only digital files, some need location shots and want prints. Our studio offers many options to personalize your portrait session and end products. Clients should expect to invest a minimum of $500 on their photo services and products. To get a detailed quote customized to your needs, contact us via the button below!


I am frequently approached by residents asking what they may or may not be permitted to drop off in respect of household and other waste.
Following a recent Waste Management Forum meeting on 19 March 2012, the following document emerged and gives very clear guidelines.
Please remember that for Ward 2, the nearest metro transfer station/TIP is situated along Strandfontein Rd between Strandfontein Rd and the Forest Hill Cemetery. Should you wish to dispose of items other than what is allowed at the transfer station, then the nearest landfill site remains the Arlington Waste Facility on Victoria Drive in Walmer.
Should you have any additional queries, please feel free to utilise the various contact details contained below.
Waste may only be disposed of at one of the licensed landfill sites or approved municipal drop-off centres/transfer stations.
Loads or items NOT accepted at these sites MUST be disposed of at Arlington or Koedoeskloof Waste Disposal Sites.