They are or were called "fold mountains" but I've not seen the term used much now because it's taken as read.
Essentially all mountains composed of sedimentary rocks above the continental basement (as I think you mean) are formed in this way, with the uplifting, folding and faulting being parts of the whole result.
The cause is the Continental Collision part of Plate Tectonics.
When land is sqeezed together it is because tectonic plate are moving and crashing into each other. When the plates ceash into each other they can create a mountain. But if they rubb up against each other they can create a earthquake.
A horizontal fold is known as a syncline. In a syncline, the youngest layers of rock are found in the center, while the oldest layers are exposed on the outer parts of the fold. This type of fold typically forms in compressional tectonic environments when rocks are squeezed together.
Capable of being pressed together or forced into a narrower compass, as an elastic or spongy substance.
pp
Petrified
folded mountains
folded mountains
Folded mountains are formed this way.
When land is sqeezed together it is because tectonic plate are moving and crashing into each other. When the plates ceash into each other they can create a mountain. But if they rubb up against each other they can create a earthquake.
no
The region in a compressional wave where coils are squeezed together is called the compression or condensation. This is where the particles are closest together, leading to an increase in pressure.
A horizontal fold is known as a syncline. In a syncline, the youngest layers of rock are found in the center, while the oldest layers are exposed on the outer parts of the fold. This type of fold typically forms in compressional tectonic environments when rocks are squeezed together.
it is compression
false
A group of molecules squeezed together is called a solid. In a solid, the molecules are closely packed and have fixed positions relative to each other.
Capable of being pressed together or forced into a narrower compass, as an elastic or spongy substance.
Rock fragments that are squeezed together tightly form a sedimentary rock called breccia. Breccia is composed of angular fragments of rocks that are cemented together by a fine-grained matrix. It typically forms near fault zones or where there has been significant rockfall or landslides.