They are canyons
young
A bay is an area that is surrounded by land on three sides. A headland is surrounded by water on three sides. Headlands usually have steep sea cliffs.
The valley have steep sides because soil and loose rocks are washed downhill after a heavy rainfall. The soil and rock also create a load in the river.
Hills are created by erosion and fault and mountains are made by 2 tectonic plates colliding
A long, narrow valley between high cliffs is a canyon. Canyons within mountains, or gorges that have an opening on only one side are called box canyons. Slot canyons are very narrow canyons, often with smooth walls.
The river cliffs are developed by erosion of the rocks by the water and rocks. The friction between the two will result slopes on the ground and after a span of time. Enormous cliffs will appear in the borders of the river. river cliffs are formed by the water eroding away the rock, and, overtime, they will create massive cliffs on the sides of the river
The slopes of the opposite sides are equal.
i believe it is a ridge if your talking about the part of the mountain that slopes down on opposite sides of a valley where the peak is the crest. :) hope that helps
Cliffs are formed when the softer rock and sediments erode away from rock formations that are more resistant to erosion, like sandstone, granite, or basalt. They are also formed by sudden geologic movement, like landslides or earthquakes along fault lines.
All streams meander to some extent. The most likely time is when flow is consistent and gradient is uniform. See Braided Stream. When a stream has eroded the steep valleys to genteler slopes, the stream flows more slowly.Now water in the stream erodes along the sides of the stream bed rather than along the stream bottom. === ===
The cliffs offered protection from from raiders.
valleys are made when a stream erodes at the sides and bottom.
Each pair of opposite sides has equal slopes.
The Anasazi
Each pair of opposite sides has equal slopes, as in every parallelogram.If all of its sides had the same slope, then they would all be parallel, andit would be difficult to construct a rhombus or parallelogram with them.
there are no such things only V shaped valleys which have sides sloping down to a river that has cut the valley out of the rock and U shaped valleys with flat bottoms and steep sides. these have been carved out by glaciers
Vales or Glens