because is he mad
syncline
Yes, rocks can be bent or overturned by the force and pressure of volcanic eruptions. Intense heat and pressure can cause rocks to deform, fold, or even fracture during volcanic activity. The extreme forces involved in volcanic eruptions can lead to significant changes in the geological structure of rocks.
An upward fold in rock that forms an arch-like structure is called an anticline. It is a type of fold in the Earth's crust where the rock layers are bent upwards in a convex shape, with the oldest rocks located at the core of the fold.
A valley of rolling hills is an example of an asymmetrical anticline fold. This type of fold consists of layers of rock that are bent in an arch-like shape, with one limb dipping more gently than the other.
fracture
because is he mad
The crest of a fold refers to the highest point or top of a folded rock structure. It is the part of the fold where the rock layers are most tightly compressed and bent upwards. The crest can help geologists interpret the original orientation and deformation history of rock layers.
a fault is a large crack in the earth. a fold is when the ground gets bent.
Fold mountains are formed from the collision of continental tectonic plates. Since neither plate subducts under the other, the colliding plates wrinkle and fold like a rug being pushed into a wall.COMPRESSION A+by ARELY
Synclines
A downward fold in a rock is called a syncline. It is a type of fold in which the rock layers are bent downward in a trough-like shape.
syncline
Yes, rocks can be bent or overturned by the force and pressure of volcanic eruptions. Intense heat and pressure can cause rocks to deform, fold, or even fracture during volcanic activity. The extreme forces involved in volcanic eruptions can lead to significant changes in the geological structure of rocks.
Fold it back the other way, there will be a crease but it'll be straight.
with the heated girth of your fat girlfriend
An upward fold in rock that forms an arch-like structure is called an anticline. It is a type of fold in the Earth's crust where the rock layers are bent upwards in a convex shape, with the oldest rocks located at the core of the fold.