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Run Off Water. Run off water is a result of water not being able to be absorbed by the surface of the ground. Gravity pulls the run off water along the.

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Presentation on theme: "Run Off Water. Run off water is a result of water not being able to be absorbed by the surface of the ground. Gravity pulls the run off water along the."— Presentation transcript:

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2 Run Off Water. Run off water is a result of water not being able to be absorbed by the surface of the ground. Gravity pulls the run off water along the ground until it hits a low point or finds a stream. Heavy rainfall = quick saturation and increased run off. Long period of rain has the same result as a heavy rainfall Steeper land = faster flow of water, less absorption, & more run off Low, gently rolling lands = slower moving water, more absorption, & less run off. Little vegetation = greater amount of run off water.

3 Tracking Run Off Natural vents & human activities can affect run off & cause problems Too much run off = rivers flood, flooding = washing away important soil Fast moving rivers = large amount of fine sand & silt, harming fish & other aquatic animals

4 Drainage Precipitation falls = works way into common river = drainage basin Falling water = flows into streams from drainage basins River systems are similar to trees

5 Ground Water Rocks with large pores allow lots of water to flow through Rocks with smaller pores allow less flow of ground water A well = man made hole in the ground that is very deep & goes pass the water table ¼ people in British Columbia get their water from a producing well

6 Glaciers Glaciers = snow & ice 2/3 of the worlds fresh water comes from glaciers Many years = snow gets very deep Glaciers covered most of northern parts of British Columbia Water normally = flowing through rivers = frozen in water Two types of glaciers = Alpine glaciers or continental glaciers Two of largest ice sheets on earth = found in Antarctica Glaciers will slide down a slope Big chunks of ice = icebergs Glaciers in British Columbia are receding


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