it erodes on its bottom
the same number of sides and internal angles but not the length of the sides.
Margins. They are what covers blank areas at the top, bottom, and sides of the page(:
A geometric diamond has 4 sides and 4 angles. The precious stone has any number of sides and angles - as the cutter determines.
six (the same number as the cube) sides/faces = 6 [1 top + 1 bottom + 4 sides] edges = 12 [4 top + 4 bottom + 4 sides] corners = 8 [4 top + 4 bottom]
it erodes on its bottom
it erodes on its bottom
it erodes on its bottom
large sediments.
a lot of things move through water the river picks it up and erodes the sides and bottom of the river
Valleys are made of rocks and soil components. Valleys occur as a result of erosion which is commonly caused by water which erodes the sides and the bottom of a valley.
the uplift of the surrounding landmass. The stream erodes downward, carving a V-shaped valley, while the landmass rises due to tectonic movement. Over time, this combination results in the formation of V-shaped stream valleys.
Most sediment washes or falls into the river as a result of mass movement and runoff. Other sediment erodes from the bottom or sides of the river
A stream is likely to meander when there is a low gradient, or slope, in the land it flows through. This slow-moving water creates curves and bends in the stream channel, causing it to meander as it flows downstream. Other factors such as the amount of sediment carried by the water and the type of rock or soil in the streambed can also influence meandering.
Yes, a valley typically has steep sides that slope down to a flat bottom where a river or stream may flow. The steep sides are usually a result of the erosion caused by the flowing water over time.
it is called a meandefill
Valleys are typically formed by a combination of erosion processes such as rivers cutting through the land, glaciers carving out U-shaped valleys, or tectonic forces creating fault-block valleys. Over time, these processes shape the landscape by wearing away the Earth's surface, leaving behind the characteristic V-shaped valleys we see today.