Valley or canyon
Heat from the sun evaporates water from the oceans. This rises and condenses to form clouds. The clods drop their moisture over land as rain, which drains into streams and rivers. All rivers eventually empty back into the oceans - and the cycle begins again!
Land formed from sediment build-up is called a delta. Deltas usually form at the mouth of rivers where sediment, such as sand and silt, is deposited as the water slows down and spreads out.
The Chickasaw were originally from the southeastern United States, primarily in present-day Mississippi, Alabama, Tennessee, and Kentucky. They lived in villages and towns along rivers and streams and often utilized the land for agriculture, hunting, and gathering. Chickasaw land was important for their survival and cultural practices.
Yes, boundaries can be formed by both land and water. Land boundaries are typically defined by physical features such as mountains, rivers, or roads. Water boundaries can be natural features like rivers or lakes, or man-made features like canals or artificial islands.
landforms are formed by volcanoes?
alluvial fans, deltas, groundwater erosion, deposition, soil on flood plains
The streams and rivers would incise (cut down into) the land in order to achieve their desired gradient.
River sources are the rain falling on high ground. Sometimes the runoff flows into streams that flow into rivers. Other times the streams run into lakes that outflow from the lakes is the source of the river. The Nile river is an example of a lake sourced river.
Runoff.
transporting pollution
rivers, lakes, streams. nd forests
When water reaches land it can flow across the land until it reaches rivers, lakes, streams or the sea.
No Antigua has only three creeks or streams.
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.
A lake, pond, reservoir, many rivers/streams, or an inland sea.
Runoff
A fluvial plain is a flat, fertile land area that is formed by the deposition of sediment carried by a river. It is typically found alongside rivers and streams and is known for its rich soil and suitability for agriculture. These plains experience periodic flooding which helps deposit nutrient-rich sediment.