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The process by which rocks are chemically altered or physically brokedn down into fragments at or near the Earth's surface |
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Break down of rocks into progressively smaller grains called detritus |
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mechanical weathering that occurs due to presure release. Sheet joints form as the pressure is released during outward expansion of the rock and form exfoliation domes |
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Role of joints in weathering |
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Increase surface area allow water to endter the rock promotes chemical weather |
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joints intersect bedding planes and eventually transform solid rock into rubble called talus |
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thermal expansion and contration |
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volume of rock changes as it heats and cools |
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rock expands more on its outside than inside. Causes rocks to break apart |
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Decomposition of rock materials by reaction with chemical reagents oxidation Dissolution hydrolysis |
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chemical reaction where an elemnt loses electrons These reactions produce sulfuric acid which forms the basis of acid rain and is the main component of acid mine drainage |
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to cause to pass into solution. -easiest type of chemical decomposition -most mienrals aren't water soluble -some minearls are especially soluble, the most important of which are calcite and halite. |
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breaking down minearls by the addition of water -mostly affects silicate minerals -water combines with CO2 to form carbonic acid |
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Factors that influence weathering |
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-Mineral stability- metastable minerals are more easily weathered -surface area- more surface area=more rapid weathering organisms- organisms may either cause mechanical weathering (root wedging) or produce natural acids taht create chemical weathering |
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Are from mechanical and chemical breakdown of preexisting rocks are by direct precipitation from aqeous solutions compntents: 1.fragments 2. chemical precipitates (salt or gypsum) 3. materials formed by biochemical processes |
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Why are sedimentary rocks important |
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preserve recordds 90% of mineral products use come from sedimentary rocks (coal, oil, sand, etc) Act as reservoirs for groundwater |
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Two broad types of sedimentary rocks |
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1. clastic or detrital- from pre-existing rocks by weathering 2. chemical and biochemical- from precipitation from aqueous solutions and/or by biochemical means |
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The conversion of sediments into rock 1. compaction and dewatering: As the weight of overlying materials increases, sediment grains are packed more tightly together, squesszing out water. 2. Lithification: Once the sediments have been tightly packed, water taht is rich in mineral components will deposit mineral cements in the remaining pore spaces |
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drawing a diagram showing the vertical and sometimes horizontal relationships among and between strata in a given region |
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stratigraphy is the term given to the study of the characteristics and attributes of rocks. Must be at least 100 m thick. |
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strata are divided up into even smaller layers. Separate, distinct layers based on certain criteria |
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Similar rocks are grouped together as |
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formation- member- a distinctive smaller unit within a formation group- a series of formations that typically are related by common lithologic attributes |
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Sedimentary rocks and geologic time |
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System: corresponds to a geologic period series: a subdivision of a system which corresponds to a geologic epoch stage: a subdivision of series, a way to refine specific times within a geologic epoch |
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Clastic Sedimentary Rocks |
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Making a clastic sedimentary rock involves 4 steps 1. Weathering 2. Erosion/mass wasting/transportation 3. deposition 4. Diagenesis/lithification |
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classification of sedimentary rocks is based on |
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1. grain size 2. shape 3. mineroalogy |
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of sediment is how far it has been transported from its source. |
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refers to the range in sizes of the sediment |
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non detrital sedimentary rocks |
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include the chemical and biochemical sedimentary rocks |
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occur in a restricted basin with episodic influx of water. -Water is evaporated faster than it is supplied and limestone, gypsum, and rock salt precipitate out |
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cross beds graded beds ripple marks mud cracks fossils |
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downslope transfer of material by graviety factors 1. saturation of material with water 2.earthquakes 3. oversteeoening of slopes 4. freeze thaw cycles |
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regolith detaches from the substrate along a glad horizone and moves downsope |
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mudflow: material is small in size debris: material contains cobble size and larger rock fragments |
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When rocks are weathered and turn into sediments any type of unconsolidated debris produced is called_______. |
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Regolith behaves in three ways |
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1. It can breakdown further and evolve "in situ" and become soil 2. mass wasting 3. can turn back into sedimentary rock |
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part of the regolith that has evolved and cna support and sustain plant life |
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how soil forms and what it is made of |
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1. the action of water 2. biological interaction air mineral matter water organic matter |
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