Weathering, Erosion, Deposition
Weathering / breakdown of rocks at or near the Earth's surface
Types of Weathering / Physical and Chemical
Physical weathering is the / breaking down of rocks into smaller pieces (sediments) without chemical change
Physical weathering is most dominant in / moist, cold conditions
What does physical weathering do? / Creates more surface area
Frost action / water seeps into the cracks, freezes and expands
Abrasion occurs when / rocks rub and become smaller and rounder in a stream or wind
Root action / roots grow into and under rocks and pry the rock apart as the roots continue to grow
Exfoliation / surface rock "peels" off due to the rock expanding and contracting from temperature and pressure changes
Chemical weathering / changes the chemical composition of the rock
Chemical weathering is most dominant in / warm, moist conditions
Where does chemical weathering occur? / On the surface of rock materials
Oxidation / when iron combines with oxygen to make iron oxide
Carbonation / carbonic acid causes minerals to dissolve away
Hydration / water weakens the rock, and it crumbles
What is the key to chemical changes? / Water
As particle size decreases / surface area increases and the rate of weathering increases
Resistant layers of rock stick out and form / cliffs or escarpments
Chemical weathering will occur most rapidly when rocks are exposed to the / hydrosphere and atmosphere
Soil develops because of / weathering and biological activity over long periods of time
Residual soil / soil that formed and stayed in the place – same substance of the underlying bedrock
Transported soil / made up of completely different material than the underlying bedrock
Soil that contains large quantities of calcium was most likely formed by the weathering of / limestone
Erosion is the / movement of sediments
Major agent of erosion / water
The 5 Agents of Erosion / Water, Glaciers, Wave Action, Wind, & Mass Movements
The primary force that drives the agents of erosion is / gravity
Stream valleys are / V-Shaped
Most of the surface materials in NY State can be classified as / transported soils
By which processes are rocks broken up and moved to different locations? / Weathering and erosion
Gravity causes water to flow / downhill
The faster the water moves / the larger the particles it can transport
As water slows down / the larger, rounder more dense particles settle out first
Stream / any body of water with a current
Stream velocity depends on / gradient (steepness or slope) and volume (amount) of water
Discharge / volume of water flowing past a fixed point in each period
Oxbow Lake / a cut-off meander
The outside of a meander bend is / fast and erodes (elbow)
The inside of the meander bend is / slow and deposits (dent)
Meander / curve in a stream
Life of a Stream | |
Youth |
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Mature |
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Old Age |
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Drainage patterns / determined by the topography of the surface and the underlying bedrock
Dendritic Pattern / looks like branches on a tree
Radial Pattern / occurs when stream flows away from a high point and looks like spokes on a wheel
Annular Pattern / occurs on an eroded dome and has a circular pattern with small tributaries going into each circle
Rectangular Pattern / occurs were drainage flows along folds and faults
Evidence of gravity erosion is / unsorted and angular (sharp) rocks at base of cliff
After mass movement rocks look / rough and angular
Which process describes the downward sliding of the rock material? / Mass movement
A landslide is an example of / mass movement
Wave action round sediments because of / abrasion
Shores are protected by / barrier islands
Beaches are formed by the / weathering of continental & oceanic rocks
Longshore drift moves / sand along the beach in the direction of the ocean current
Barrier Island / a long, narrow island running parallel with the mainland made up of mostly sand
Barrier Islands are made by the action of / wave currents and wind that distributes the sand which protects the mainland from erosion
Jetties and Groins are / beach protection structures that protect against longshore drift
Glacier / large, very slow-moving mass of ice
Gravity causes a glacier to move / downhill
Glacial landscapes show / U-Shaped Valleys, erratic (large boulders), kettle lakes, moraines, drumlines and scratched bedrock (striations)
Glacial and gravity deposition is / unsorted (all mixed up called till)
Glaciers form in / high latitudes and high elevation
Esker / long winding ridge of sorted sands and gravel
Moraine / material left behind by a moving glacier
Terminal Moraine / moraine ridge that makes the marks the maximum limit of glacial advance
Recessional Moraine / small ridges left as a glacier pauses during its retreat
Outwash Plains form as / a glacier melts and rivers carry small sediments (sorted) away from the glacier
Drumlins / hills of sediment that have been streamlined by glacier flow
Kames / moundlike hill of poorly sorted drift deposited at or near the end of a glacier
Kettle Lake / large, water filled pothole left in the ground by a receding glacier
Glaciers advance from the / north, formed Long Island, left sand and gravel (moraines)
Wind Erosion creates / sand dunes, the windward side of a sand dune has a gentle slope
Deposition is the / dropping or stopping of sediments after erosion
Round, large, more dense particles settle out / faster than angular, small and less dense particles
Sorted sediments settle out in a / distinctive order
Unsorted sediments are dropped in / no particular order
Water and wind deposits are / sorted and layered
Glacial and gravity deposits are / unsorted and not layered
Horizontal Sorting / occurs when a stream enter a large body of water , velocity slows down, larger particles settle out first
Vertical Sorting / sorting of sediments from bottom to top, large round and dense particles settle out first at the bottom
When a river enters the ocean / it slows down, deposits and forms a delta
Watershed is a / geographic area where all the rainwater flows into a river
Tributary / creek or stream that flows into a larger body of water
Delta / triangular shape of deposited sediment of the mouth of a river
Drainage Basin / area where water flows downhill into one large body of water
Deltas form when / deposition is greater than erosion