increases the vertical distance between the source and destination increasing energy.
The lava flows into a volcano
Streams can't erode their channels endlessly. there is a lower limit to how deep can a stream erode. Base level is the lowest point to which a stream can erode its channels.
Streams can't erode their channels endlessly. there is a lower limit to how deep can a stream erode. Base level is the lowest point to which a stream can erode its channels.
If you lower a stream base level it will cause a down cut. In some cases this is a good thing.
A good example of Erosion would be like after a hard rain, the rain drains and makes a little crevice like a little stream that's lower than the surrounding dirt.
Such a cave is called "abandoned" or "fossil"; a stage reached when it loses itsr formative stream. Either a series within the cave is abandoned when the stream cuts down to a lower level within the limestone; or the whole cave is abandoned when surface erosion removes or diverts the stream feeding the cave entirely. Fossil caves local to me (on the South coast of England) have entrances some 100 to 200 feet above sea-level, in sea-cliffs, because the erosion here, influenced by sea-level changes in the present Ice Age,has both cut the coast back and totallyremoved the caves' original catchment area!
The results of a lower base lever for rivers and streams is the sea level falls and the land rises. The base level is the level below which a stream cannot erode.
The normal pH of a stream ranges between 6.5 to 8.5. A pH value that is higher or lower than this range would adversely affect the survival of the aquatic organisms living the stream.
No. The jet stream is in the upper troposphere and lower stratosphere.
scour, or eolian erosion
Gravity is what causes a river to flow from higher to lower elevation. A river travels at a faster speed the higher the elevation and will typically cause greater erosion.
The river valley becomes flat in its lower course due to the levels of erosion occurring in the river itself. In the upper course, the river's energy is used for vertical erosion(downward erosion) in order to get to sea level. That's why you see steep V-shaped valleys or Gorges being formed. However, in the lower course when the river is at sea level, a lot of this erosion becomes lateral(horizontal) which is why you see rivers becoming a lot wider in the lower course. Therefore, because the river is no longer eroding downwards there's no longer a difference in height between it and its valley, so the river valley becomes flat.
External forces are the forces that can lower the level of the land by washing it away and.this.is called denudation and rise the level this.is called decomposition Denudation can be weathering and erosion