This is the water cycle.
Water flows downhill. Contour lines show the slope of the landscape, and the direction a stream must flow.
Stream gradient, or the slope of the stream channel, affects stream velocity by influencing the speed at which water flows downstream. A steeper stream gradient typically results in a faster water flow velocity, as the force of gravity pulls water downhill more strongly. Conversely, a gentler stream gradient leads to slower water flow velocity.
it evaporates and then it condensate after that it rains in the oceans and seas.
Runoff is the water flowing downhill across the surface of the Earth.
The terms are typically synonymous : )- the opposite of a perennial stream which flows year round.
Yes, it is correct.
A lava flow is a stream of molten rock that moves downhill from an erupting volcano.
Water flows downhill. Contour lines show the slope of the landscape, and the direction a stream must flow.
Evaporation of water occur at any temperature at the surface of a body of water.
A stream is typically created when water flows naturally downhill due to gravity, forming a channel or watercourse. This can occur from sources such as springs, melting snow, or rainfall. As the water continues to flow, it erodes the ground and shapes the stream over time.
the difference in velocity is mostly due to the great efficiency of the large downstream channel.
When water flows downward what will it posses
That is a glacier. Glaciers form from compacted snow that has accumulated over time and flows downhill under the force of gravity.
An avalanche
runoff
Water from waterfalls drops into pool of water which then flows as a river continuing downhill to the sea.Then it evaporates into clouds, falls as rain onto high ground, and flows down from the high ground into rivers which could possibly fall from that same waterfalls again.
In this investigation, students explore river and stream erosion. Precipitation (rain) that falls to the Earth's surface either soaks into the ground, evaporates, or flows across the land. Water that flows across the land runs downhill. Along the way, it can pick up and carry sediment ranging from fine clay to coarse sand or gravel. As the water runs downhill, it cuts into the soil, forming channels called gullies. When gullies reach a low-lying area, they merge together, forming a larger stream. Streams merge together to form larger streams or rivers. Most sediment carried downhill eventually ends up in a stream and is carried away. In this way, streams affect more of the Earth's surface than any other agent of erosion. The amount of sediment a stream can carry depends on the speed and size of the stream. The speed of the water in a stream depends on its slope. The steeper the slope, the faster the water moves. Fast-moving or large streams can carry more sediment than slow-moving or small streams.