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Review: Erosion/ Deposition
Main Topics: Ground Water Soil Horizon Weathering Erosion Deposition Glaciers Water NY Landscapes
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How does Groundwater work?
Water falls to the ground and infilitrates the soil. It finally stops when it hits the bedrock.
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Characteristics of the soil
Permeability: How quickly water passes through a surface (Larger the better) Porosity: open space in the soil (size doesn’t matter) Capillarity: upward movement of water in the ground (Smaller the better) Runoff: water found on the surface
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What is the soil horizon?
Soil Horizon is a profile of the ground and how the bedrock is transformed into fertile soil. A: Topsoil: Fertile: Humus/ organic materials B: Middle: Mineral Enriched C: Bottom Solid Bedrock
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What is weathering? Breakdown of a substance. Physical-smaller pieces
Climate: Cold & Moist Chemical- change Climate: Warm & Moist
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What is Erosion? Erosion: Movement of materials Chief Agent: Water
Rivers move sediments Table pg6 Move fastest in straight middle Curve fastest outside bend
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ESRT pg 6
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What is deposition? Deposition:Settling of Sediments Factors:
Size, Shape, Density Horizontal: Largest sediments closest to the mouth Vertical: Largest sediments on the bottom
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How are landscaped shaped?
By the deposition and erosional processes.
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How do places that were affected by Glaciers Look?
Glaciers: Unsorted sediments in ground Rocks have striations (Scratches) Valleys are “U” Shaped
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How do places that were affected by water look?
Water: Sediments sorted. Either vertical or horizontally Sediments are smoother, rounder and smaller Valleys are “V” Shaped
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