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Ks3 s

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Some rocks may be different shapes and sizes as they be changed by the conditions in their   environment.              
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The breakdown of rocks into smaller fragments is called   weathering.              
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In alphabetical order, the 3 types of weathering are;   biological weathering, chemical weathering and physical weathering.              
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Freeze-thaw weathering is the repeating of both   freezing and thawing. This is done to both   water and ice in the   gaps inside   rocks. When the water freezes, turns to ice and expands making the gaps   larger and eventually causes pieces of rocks to   break away.    
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Often with freeze-thaw weathering, the water off freezes during   day, while it thaws during   night. This process is   repeated until the fragment of rock   breaks off.        
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Freeze-thaw weathering is a type of   physical weathering.              
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Exfoliation weathering or   onion skin weathering is the repeating of both   heating and cooling of   rocks, which causes the surface layer to   flake off, possibly leading to that rock   splitting.      
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With exfoliation weathering, often the heating is done during the   day, while the cooling is done during the   night.            
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Exfoliation weathering is a type of   physical weathering, where as that rock keeps expanding and   contracting, pieces of that rock's surface begin to   flake and eventually   fall off.        
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With exfoliation weathering, during the day, the surface of that rock is heated by the   sun, causing that rock to   expand. During the night, instead of being heated, that rock   cools and then   contracts.        
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With biological weathering, plant roots and   shoots can get into minute   cracks in   rocks. As the plant grows, roots and shoots can push their way through the   rock, which (in those rocks) forces   cracks. The growth of cracks in this way causing small pieces of rock to   break off.    
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Chemical weathering is the break-down of   rocks when there are   chemical reactions between   acid rain and   certain minerals in   rocks. Some types of rock are easily weathered by chemicals. For example, limestone and chalk are made of a mineral called calcium carbonate; when acidic rainwater falls on limestone or chalk, a chemical reaction happens: new [] substances are formed in t   soluble. These are washed away and the rock is    
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Rainwater is naturally acidic because rainwater reacts with   carbon dioxide in the   air to form   carbonic acid.This type of acid rain is weakly   acidic and reacts   slowly with      
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The burning of fossil fuels produces both   oxides of Sulphur and Nitrogen which make rainwater more   acidic. This type of acid rain reacts   quickly with   minerals and weathers rock more        
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3 ways that rock fragments can be transported are(in alphabetical order);   glaciers, rivers and strong winds. Rivers and stream and the like moving pieces of rock is called   transport. [] flowing rivers can transport large rocks, but [] moving rivers can only transport tiny pieces of rock.   fast---slow. As the pieces of rock are carried along by the water, they bash against each   other and the river   bed, thus, they eventually [] []   wear away. They become s[] and more r[].   They become smaller and more rounded.  
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Deposition occurs when pieces of weathered   rock sink to the   bottom of either the   river bed or sea forming   sediment. Dead creatures can get trapped in   sediment and form   fossils. It is considered that the time it takes for something to become a fossil is   10,000 years.  
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Sediment, such as sand and silt is deposited in   layers. The build up of layers is called   sedimentation. The layers become compacted to form   sedimentary rock. The distinct   layers of   rock are related to the   time intervals at which there is an occurence of   sedimentation.  
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The 5 parts of the cycle of which rocks partake are (in consecutive order);   weathering, erosion, transportation, deposition and sedimentation.              
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The process of weather and transportation is known as   erosion.              
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Sometimes, metamorphic rocks are formed when rocks are close to some   molten magma, and so get   heated. Metamorphic rocks may form from rocks heated by   magma.When a metamorphic rock is formed under pressure, its crystals become arranged in          
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Wind, rain and waves can all cause physical weathering. The wind can blow tiny grains of sand against a   rock, that wear the rock   away and [] it   weather. [] and [] can also wear away rock over long periods of time   Rain and waves.        
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[] is the movement of the broken pieces away from the site of weathering.   Erosion              
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With freeze-thaw weathering, water enters the   gaps inside   rocks, then when the temperature reaches 0° or   less, the water in consecutive order   freezes then expands leading to rock fragments   breaking off.      
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What happens to weathered rock? The fast moving water picks up large pieces of   rock, which are   eroded as they are   carried along, then as the river widens out, large pieces of   rock are deposited by the   slow moving water. Most of that rock fragments are deposited at the   mouth of the river where it is both   wide and slow-moving.  
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