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Surface water- Oceans, Lakes, Ponds, Swamps, Rivers, Streams... Groundwater- Aquifers, Caverns...
it has fresh soil for planting freash streams for fishing and timber for building ships
you mean jet streams...or thermals?
The landscape between Dallas and San Antonio is gently rolling hills or flat, broken by streams which generally flow to the southeast. Much of it is farmland, with forested areas near water sources. The landscape is increasingly urbanized, however. Only one county on the direct route between Dallas and San Antonio is not currently part of a metropolitan area.
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River hydraulics involves flowing water and its impact on the landscape. This includes the hydraulic characteristics of streams and rivers ranging from dam break analysis to sediment movement analysis.
meandering
they lived by rivers and streams
Glaciers can form various landscape features, including U-shaped valleys, cirques, aretes, and moraines. These features are created as glaciers erode and deposit material as they flow over the land.
They erode the landscaping around them.
Rapids and lots of whitewater
the three geographical characteristics of virginia are moountains and waterfall and hills xoxo
you stink is my answer
Boreal forests, also known as taiga forests, are found in northern Europe, Asia, and North America where cold lakes and streams are part of the landscape. These forests are characterized by coniferous trees, such as spruce, fir, and pine, and have adapted to cold and harsh conditions. They are an important habitat for various wildlife species like bears, wolves, and moose.
Sedimentation and erosion will lead to a downward path and deepening bed of streams as one characteristic. In early stream erosion, the erosive activity is primarily vertical.
In the United States there is more than 25000 River =]
Some common characteristics of old age streams include decreased flow rates, reduced water volume, increased sedimentation, and a shift in dominant plant and animal species. Additionally, old age streams may exhibit wider and shallower channels, more frequent meandering, and a decrease in overall geomorphic activity.