LANDSCAPES – Development and Change
Major Points - Landscape characteristics are the result of - interaction of forces of crustal movement - climate, - human activities - time
Underlying bedrock determines landscape
Landscape regions can usually be identified by the elevation of the region (relief) There are 3 types: Mountains, plateaus and plains.
Mountains High elevation Deformed rock structures due to forces of mountain building.
Plateaus Medium to high elevation Sedimentary rock forms base
Plains Low elevation Horizontal rock layers rock layers Landscape regions tend to be separated by mountains, large bodies of water and other natural boundaries.
What Forms Landscapes? - Two major forces oppose each other : Uplifting forces/Constructive – mountain building, -continental accretion (caused by earthquakes, volcanoes, folding, faulting)
Leveling forces/Destructive – weathering and erosion. Creates an equilibrium or balance
Climate Arid vs Humid Arid – jagged, angular, dry Humid – moderate to high precipitation - rolling, low slope, grassy, well-defined soil profiles.
Old vs New Old – gentle rolling hills, worn away, oxbow lakes. Ex. New York New – jagged mountains, more angular, steep slopes Ex. Pacific Mt. Ranges: Cascades and Sierra Nevada
Bedrock Effects how the landscape looks according to its resistance to weathering and erosion. Cliffs: results from rock that varies in rock resistance – resistant rock juts out in a series of layers due to composition – resists weathering.
Water for Stream Flow A stream gets its water from rainfall, runoff and overland flow. How quickly a stream gets water depends on:gradient, vegetation, distance, urban vs rural areas… Watershed Geographic are that drains into a specific stream of body of water.
Stream Drainage Patterns Patterns made as stream crosses land. Result of underlying bedrock, gradient. There are 5 General Types: DARRT
Dendritic – treelike, uniform
Annular – eroded hill areas
Radial – central point drainage
Rectangular- found in regions where faulting occurred.
Trellis - develop where there is strong structural control upon streams because of geology.