No. It is called an unconformity. A fault is a fracture along which blocks of rock have moved relative to one another.
That would be "sedimentary rock". Sedimentary rock is formed from the accumulation and compression of sediments, including fragments of igneous rock that have been weathered and eroded.
A line of weakness in which sedimentary rocks can be separated is called a bedding plane. This is where layers of sediment have accumulated and can be easily split or eroded along this plane due to variations in sedimentary deposition.
Sedimentary rock forms from the layering of eroded rock material, which accumulates and undergoes compaction and cementation over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
The process by which rocks are replaced as they erode from Earth's surface is called deposition. Deposition occurs when eroded rocks and sediments are transported to a new location and settle out of the transporting medium, such as wind or water, to form new layers of sedimentary rock.
The contact between an old eroded rock surface and a new rock layer is typically referred to as an unconformity. Unconformities represent gaps in the geologic record where erosion or non-deposition has occurred, leading to a break in the sequence of rock layers. These features are important for understanding the relative timing of events in Earth's history and can provide insights into past environmental conditions.
An angular nonconformity occurs when younger sedimentary rock layers are deposited on top of older, tilted or folded sedimentary rocks that have been eroded. This geologic event typically involves tectonic activity, such as folding or faulting, which alters the orientation of the older rocks. After this deformation, erosion removes the upper layers, and then new sedimentary layers are deposited horizontally on top of the eroded surface, creating the angular nonconformity.
A dis-conformity is an unconformity representing a period of erosion or lack of deposition in a sedimentary rock section.
That would be "sedimentary rock". Sedimentary rock is formed from the accumulation and compression of sediments, including fragments of igneous rock that have been weathered and eroded.
Sedimentary rocks always originate at the surface of the solid Earth. They form from the accumulation and lithification of weathered and eroded materials such as sand, silt, and clay.
It is called an erection.
The presence of geodes appearing on the surface of a given locality is dependent on the geologic history of that area. Geodes are usually found in areas of exposed and eroded sedimentary rock. The shell of the geode, often quartz, weathers less vigorously than the entrapping rock, usually calcitic or dolomitic limestone. In northern lattitudes, glacial deposits may have covered up the geodes and sedimentary rock, or perhaps the sedimentary rock layer did not exist previously or has eroded away completely.
Sedimentary rocks are by definition composed of little pieces of eroded rocks. So, yes!
A line of weakness in which sedimentary rocks can be separated is called a bedding plane. This is where layers of sediment have accumulated and can be easily split or eroded along this plane due to variations in sedimentary deposition.
It can change when it is eroded and weathered.
The depositing or placing of eroded material is called sedimentation. This process occurs when eroded particles settle and accumulate in a new location, often leading to the formation of sedimentary rocks over time.
Sedimentary rock forms from the layering of eroded rock material, which accumulates and undergoes compaction and cementation over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
The grain of sand becomes a sedimentary rock when it gets erosion and is deposited on the bottom of a body of water. Then the eroded sand builds up and becomes a sedimentary rock if there is enough eroded sand.