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Geog 101: Chapter 3 Quiz
Geog 101: Chapter 3 Quiz

... hills, plains) accumulate at lower elevations (such as swamps and ocean bottoms)? 10. Where are shields located? 11. Near a convergent plate boundary, rocks fracture because they are compressed: such fractures are what kind of faults? 12. During dry periods, most of the water flowing into streams is ...
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Chapter_14_Notes

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Release of Strain Energy as a Mechanism for the Mechanical
Release of Strain Energy as a Mechanism for the Mechanical

... SIR, Processes of weathering have been subdivided by many authors into two main groups: mechanical and chemical, with organic agencies falling within both these realms. Both mechanical and chemical factors such as exfoliation, frost heaving, solution etc., which arc considered to be possible mechani ...
Geology - s3.amazonaws.com
Geology - s3.amazonaws.com

... metamorphic rock- rock that has been changed due to pressure and heat sedimentary rock- rock formed from sediments that are pressed together weathering-process by which rocks are broken down and changed by exposure to environmental conditions (chemical or physical) ...
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... ______________________ them. Most fossils are found when living things are buried by sediment. The sediment ______________________________________________________________ _____________________________________________________________. Most fossils form from animals or plants that once lived in or nea ...
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Name: Pd

... METAMORPHIC ​ rocks.  12. Solidification (COOLING AND CRYSTALLIZING) of molten materials forms ​ IGNEOUS ​ rocks.  13. Deposition and burial of sediments forms ​ SEDIMENTARY ​ rocks.  14. Deposited sediments may be particles of which types of rock?​ ...
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...  Weathering causes rock to be eroded at the earth’s crust.  Erosion is both a physical and chemical process. Chemicals dissolved in water tend to break down the less resistant minerals (mafic minerals, micas, etc.) and leave resistant minerals (such as quartz and feldspar) behind. Fragments of roc ...
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... process repeats, the crack gets larger. Eventually, the rock can split. Temperature changes to the rock's surface may also cause weathering. When the rock's surface gets hotter, it expands, or grows larger. When it gets colder, the surface contracts, or gets smaller. Some scientists think that many ...
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... As magma moves up through surrounding rock it may modify the rocks near it. It may melt some rock (assimilation). However, even if the magma doesn’t melt the rock, it may subject rock to high temperatures. This type of metamorphism occurs at high temperature but not necessarily high pressure. Effect ...
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... Slieve Foye – there is a noticeable change in the appearance of the mountain at the change in geology. Both of these rocks are intrusive rather than extrusive or volcanic, meaning that they cooled and hardened from magma below the surface, but it is likely that there was volcanic activity, much like ...
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Chapter 11 - Geobiology
Chapter 11 - Geobiology

... Volcanoes release hydrogen sulfide gas. Tectonic processes uplift rocks, and weathering breaks down sulfurbearing minerals. ...
Due Date_________________ Test Date
Due Date_________________ Test Date

... b. Sedimentary Rock – forms when particles of rocks and or the remains of plants and animals are pressed and cemented together (forms in layers below the surface) c. Metamorphic Rock- is formed when an existing rock is changed by heat, pressure, or chemical reactions (most form deep underground) 3. ...
Sedimentary and Metamorphic Rock Formation and Characteristics
Sedimentary and Metamorphic Rock Formation and Characteristics

... 1) ______________________________ - associated with __________ temperatures and pressures 2) ______________________________ - associated with __________ temperatures and pressures Types of Metamorphic Rock 1) _________________________________ ...
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Save 0 - Science Lec | Home
Save 0 - Science Lec | Home

... fracturing and exfoliation of the rocks. The surface of the rock expands more than its interior. ...
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Weathering



Weathering is the breaking down of rocks, soil and minerals as well as artificial materials through contact with the Earth's atmosphere, biota and waters. Weathering occurs in situ, roughly translated to: ""with no movement"" , and thus should not be confused with erosion, which involves the movement of rocks and minerals by agents such as water, ice, snow, wind, waves and gravity and then being transported and deposited in other locations.Two important classifications of weathering processes exist – physical and chemical weathering; each sometimes involves a biological component. Mechanical or physical weathering involves the breakdown of rocks and soils through direct contact with atmospheric conditions, such as heat, water, ice and pressure. The second classification, chemical weathering, involves the direct effect of atmospheric chemicals or biologically produced chemicals also known as biological weathering in the breakdown of rocks, soils and minerals. While physical weathering is accentuated in very cold or very dry environments, chemical reactions are most intense where the climate is wet and hot. However, both types of weathering occur together, and each tends to accelerate the other. For example, physical abrasion (rubbing together) decreases the size of particles and therefore increases their surface area, making them more susceptible to rapid chemical reactions. The various agents act in concert to convert primary minerals (feldspars and micas) to secondary minerals (clays and carbonates) and release plant nutrient elements in soluble forms.The materials left over after the rock breaks down combined with organic material creates soil. The mineral content of the soil is determined by the parent material, thus a soil derived from a single rock type can often be deficient in one or more minerals for good fertility, while a soil weathered from a mix of rock types (as in glacial, aeolian or alluvial sediments) often makes more fertile soil. In addition, many of Earth's landforms and landscapes are the result of weathering processes combined with erosion and re-deposition.
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