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Unit 4: Fresh Water Surface Water

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Presentation on theme: "Unit 4: Fresh Water Surface Water"— Presentation transcript:

1 Unit 4: Fresh Water Surface Water
Fresh vs. Salt Water River Systems

2 Background Information on Water
Water = largest agent (cause) of erosion Earth’s water is categorized by its salinity: Fresh water = 3% Salt water = 97% Divided into surface and ground water

3 Uses of Freshwater Agriculture/Irrigation
Uses the most fresh water (globally) Growing crops and raising animals Reduces amount available for natural ecosystems Industry/factories Drinking Must be purified to make potable water

4 Uses of Freshwater Transportation Recreation Enjoyable activities
Changes/reduces natural habitat Can be polluted by fuels, waste, & other substances

5 Part of the Cape Fear River Basin
Parts of River Systems Part of the Cape Fear River Basin 1 River basin: area of land, streams, tributaries that all drain into 1 river Many watersheds: areas of land that drains into 1 small water body (stream, tributary, pond, etc) Aquifers: underground areas of high permeability where water is stored

6 River Characteristics: Channel Shape vs. Age
Straight & Steep Youngest—little edge erosion Gently Sloped & Meandering (aka lots of curves/bends) Older—time for erosion to make the curves Flat with Oxbow lakes (aka crescent-shaped lakes along edge) Oldest—time for erosion to make bends and then block them off)

7 River Characteristics: Headlands vs. Mouth
Rivers flow from high to low elevation Headlands Start of river in mountains Steep, narrow, straight, V-shaped channel Cold, fast-moving water Mouth End of river as it joins a lake or ocean Flat, wide, meandering, U-shaped channel Warm, slow-moving water

8 River/Stream Characteristics: Load
How much sediment the stream can move: In solution/Dissolved Load—dissolved particles throughout water Suspended Load—particles carried along in the water Bed Load—particles that bounce/drag along the bottom of the river Bed-on bottom

9 River/Stream Characteristics: Load
Load capacity depends mostly on river velocity (aka speed) Faster water moves more sediment (and slower moves less)


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