I think the answer you are looking for is bedrock.
Hope I helped..
If I did, your welcome :)
When magma flows horizontally along rock layers, it can form a feature called a sill. Sills are tabular igneous intrusions that are parallel to the surrounding rock layers. They are typically formed when magma is injected between existing rock layers and cools and solidifies underground.
Groundwater
A rock that can yield a significant amount of water is called an aquifer. Aquifers are underground layers of rock or sediment that can hold and transmit water. They are important sources of fresh water for drinking, irrigation, and other uses.
A fold where the youngest rock layers are in the center is called an anticline. In an anticline, the rock layers are folded upwards, creating a convex shape with the oldest layers on the outside and the youngest layers in the center.
The layers of any sedimentary rock are called strata.
Groundwater is the term used to describe water that fills in cracks and spaces within underground soil and rock layers.
An aquifer Hope that helps!!!
Yes, a dike forms when magma intrudes into existing rock layers and solidifies. As the magma cools and solidifies underground, it creates a vertical or near-vertical sheet-like body of igneous rock that cuts across the existing rock layers.
The underground water that fills opening in soil and cracks in layers of rocks is called ground water.
The underground water that fills opening in soil and cracks in layers of rocks is called ground water.
The layers of rock form a dome called a laccolith
insular
A bend in rock layers created by pressure is called folding. It refers to a ductile behavior in which planar or flat layers of rock bend in response to stress.
Aquifers are underground layers of rock or sediment that hold water. They can be made of various materials such as sand, gravel, or porous rock that allow water to pass through and be stored underground.
stratification
Groundwater is water that is stored underground in the pores of rock and sediment layers. It fills the spaces between particles of soil, sand, and gravel and flows through underground formations called aquifers. Groundwater is a vital natural resource that supplies drinking water to many communities worldwide.
In the same way, water underground trickles down between particles of soil and through cracks and spaces in layers of rock. People can obtain groundwater from an aquifer by drilling a well below the water table.