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Compare. Igneous Rock. Sedimentary Rock. Clastic Sedimentary Rock. Sedimentary Rock. How do those layers form? Order or process:. Weathering. Erosion. Deposition. Cementation & Compaction. Mechanical Weathering. Disintegration /rock broken into smaller pieces Frost Action
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Compare Igneous Rock Sedimentary Rock
Sedimentary Rock • How do those layers form? • Order or process: Weathering Erosion Deposition Cementation & Compaction
Mechanical Weathering • Disintegration/rock broken into smaller pieces • Frost Action • Abrasion (river, glacial, sandy environment) • Plants and Animals #2
Chemical Weathering • Decomposition-rock’s minerals are changed into different substances. • Acid Rain • Oxidation • Hydrolysis • Caves
Which minerals are susceptible? • Chemical Weathering • Calcite • Mechanical Weathering • Quartz, angular minerals
Chemical WeatheringWhat affects the rate? Faster Chemical Weathering – Warm and Moist climate Faster Physical Weathering – Cold and Wet Climate
Erosion • The transport of sediments/particles from a weathered rock by • Water • Wind • Glacier • Gravity
Water • Distinguishing Characteristics: • rounded edges
Wind • Distinguishing Characteristics • Flatten sand surfaces: Sand dune
Glaciers • Distinguishing Characteristics • Striations-special scratch by minerals
Effects of Erosion Landslide Mudslide
Evidence of Glacial Erosion U Shape Valley
Factors of Deposition • Size • Density • Shape
Two types of deposition • Water - sorted • Glacier - unsorted
Alpine Glacier • Slow moving stream of ice that flows within valley walls
Arrete Horn cirque
Continental Glacier • Glacier that covers a large part of a continent • Ex: Greenland, Antarctica
Moraine and Till Till - Unconsolidated and unsorted rock material that is deposited by a retreating or melting glacier Moraine – The accumulation of glacial till
Drumlin • Elongated whale-shaped hill formed by past glacial action as it moves over the till
Drumlins in NYS • South ends of the Finger Lakes - northeast of Ithaca at the northern end of Cayuga (Rochester to Syracuse)
Erratics • A large boulder that have been transported into an area by a glacier
Kettles and Kame • Hollows left behind by melting ice as the last remnants of glaciers disappear
Kame • Small coned shaped hill of sand and pebble. that are deposited by stream into the kettle
Complete Illustration • When glacier melts, deposits slump down at the side and form long ridges - ESKER