it forms a sedimentary rock
Folds are the when the rock layers bend. Faults are breaks in the rock layers. Folds are called anticlines and synclines. Faults are called reverse faults, normal faults, or strike-slip faults.
if it is a sedimentary rock the fossils get cemented together
An anticline is a fold in which the older layers of rock are on the inside. A syncline is a fold in which younger layers are on the incline. Usually anticlines bow upwards while synclines bow downwards.
Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.
When rock layers are folded, a geological fold happens. These folds form under various conditions such as stress, hydrostatic pressure, pore pressure, and temperature gradient.
The compressional stress can overcome the strength of the cementing material, or fracture the bonds between the crystalline structure of the rock.
An unconformity between parallel rock layers is a gap in the geologic record where erosion has removed some rock layers before new ones were deposited on top. This results in a lack of continuity in the rock record, representing a period of geologic time that is not preserved in the sequence of rock layers.
The force that causes rock layers to crumple and fold is mainly tectonic forces, such as compression. When two tectonic plates collide or move toward each other, the rocks in between experience intense pressure, leading to deformation and folding of the rock layers.
When rock layers bend or buckle, it results in the formation of folds, which can create various geological structures such as anticlines and synclines. This deformation typically occurs due to tectonic forces, such as compression, acting on the Earth's crust. The bending can affect the orientation of the rock layers and may also lead to the development of faults if the stress exceeds the rock's strength. Overall, such processes are key to understanding the geological history and structural features of an area.
fold mountains form
Fols
read it on a book:)HAHAHAHA
Layers of rock are called strata or beds. These layers are formed over time through various geological processes like sedimentation, erosion, and compression. Studying these rock layers can provide valuable information about Earth's history and past environments.
The boundary between older rock layers and newly deposited rock layers is typically marked by a disconformity. This type of unconformity occurs when there is a period of erosion or non-deposition that results in a gap in the geologic record, with the older layers being relatively horizontal. The newly deposited layers sit above the eroded surface of the older layers, indicating a break in the geological time.
They deform, first elastically then plastically.
A sill is a slab of volcanic rock formed when magma squeezes between layers of rock. It is typically horizontal and parallel to the surrounding rock layers. Sills are distinguishable from dikes, which cut across the rock layers.
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.