compression
Folded mountains. These mountains are formed when tectonic plates collide and the layers of rock are pushed together, creating folds and wrinkles in the Earth's crust. Examples include the Himalayas and the Alps.
because chalk is a type of rock which crumbles.
Gravity causes rock to fall away from steep mountains or cliffs and even by Landslides.
Fold mountains are defined as mountains created by the bending of rock layers. Volcanic mountains are mountains created by breaks in the Earth's crust. In Canada, there are many examples. For example, the Appalachian Mountains and the Rocky Mountains are fold mountains. The Canadian Shield and the coastal ranges along the North American west coast are examples of volcanic mountains.
Rock layers that bend and buckle are called folds. Folds are caused by tectonic forces that apply pressure to the rocks, resulting in deformation.
When plates slowly collide, they can form bended rock layers called folds. These folds can take various shapes such as anticlines (upward-arched folds) and synclines (downward-arched folds).
Well, mountains are formed mostly with folding and sometimes with volcanic eruptions. MOUNT EVERST was formed by the folding of the ocean. Folding is when the earth's crustal plates start to push together to form a mountain.
When rock layers are deformed into folds or ripples, it is called deformation or folding. This can occur due to tectonic forces, such as compression or extension, causing the rocks to bend and deform.
"Folding" is the term that describes the bending of rock layers due to stress.There are different types of Folds and these include:Anticlinal Folds: This is when the rock layers have an upward-arching folds.Synclinal Folds: This is when the rock layers have a downward, trough-like folds.Monoclinal Folds: This is when both rock layers ends are horizontal.
These bends in rock formations caused by tectonic plate collision are known as fold mountains. These mountains form when rock layers are squeezed and pushed together, resulting in folds such as anticlines and synclines. Examples include the Himalayas and the Andes.
the olmypic mountains is a sedmetery rock. the olmypic mountains is a sedmetery rock.
Both anticlines and synclines are folds in rock layers formed by compression. Anticlines are upward-arched folds characterized by oldest rocks in the core, whereas synclines are downward-arching folds with youngest rocks in the core. They both result from tectonic forces squeezing and deforming the Earth's crust.