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Published byBlaise Reynard Kennedy Modified over 9 years ago
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NS 1300 Emergence of Modern Science Earth’s Water
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Hydrologic Cycle
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Rivers and Streams Watershed Climate Terrain Rainfall Water always flows downhill
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Life Cycle of a Meandering River Degradational Stage Tributaries River Channel Balanced Stage Point Bars Levees Flood Plains Aggradational Stage Distributaries Deltas Terminal Stage Stream Piracy
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Drainage Patterns Dendritic Rectangular Tellis Raidal
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Erosional Features Meanders Oxbow Lakes Cut Banks Terraces Transgressive Sequences Regressive Sequences
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Depositional Features in Humid Regions Point Bars Levees Flood Plains Deltas
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Coastal Erosion Coastal Features are Ephemeral Subsidence Shoreline Erosion Jetties Dikes Sea Walls
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Depositional Features in Arid Regions Alluvial Fans Bajadas Playa Lakes
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Groundwater Aquifers Artesian Wells Caves Karst Topography
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Glaciers Alpine Glaciers Piedmont Glaciers Continental Glaciers
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Alpine Glaciers Hanging Valleys Cirques Aretes Horns Moraines
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Continental Glaciers Moraines Lateral Terminal Outwash Plain Drumlins Kettle Lakes
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Ocean Floor Continental Shelf Continental Slope Submarine Canyons Deep Sea Fans Marginal Plateaus Continental Rise Abyssal Floor Abyssal Plains Abyssal Hills Abyssal Rise Seamounts
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Ocean Ridge System Mid-Ocean Ridges Rift Valleys
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Deep Sea Trenches Subduction Zones Back-Arc Basins Clastic Wedges
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Biological Oceanography Plankton Nekton Diurnal Migration Match-Mismatch Hypothesis Benthos Marine Snow Photic Zone Thermocline
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Chemical Oceanography Salinity Heat Budget Residence Time
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Physical Oceanography Thermohaline Circulation AABW ABW Coriolis Effect Currents Gyres
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Sea Level
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Quiz 1. T or F, a watershed is the source of a streams water. 2. T or F, subsidence occurs when ground water is removed. 3. T or F, a terminal moraine occurs along the sides of a flowing glacier. 4. T or F, plankton are organisms that can actively swim against a current. 5. T or F, the salt in the oceans comes from the weathering of rocks on land.
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