A crevice, possibly? That's the only term I know
A gap in the geological record in a body of rock is called an unconformity.
A vertical gap in limestone is called a grike. The remaining blocks of rock are called klints. The cracks in limestone are called joints.
Unconformity. An unconformity represents a gap in the geologic record where erosion or non-deposition has led to a break in the sequence of rock layers.
Any gap in age of rock between rock layers is called an uncomformity. An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
A gap in an area's geologic history is called an unconformity. This represents a period of time where rock layers are missing due to erosion or non-deposition. Unconformities can help geologists understand the timing and duration of geological events.
A gap in the geological record in a body of rock is called an unconformity.
unconformities
A vertical gap in limestone is called a grike. The remaining blocks of rock are called klints. The cracks in limestone are called joints.
Unconformity. An unconformity represents a gap in the geologic record where erosion or non-deposition has led to a break in the sequence of rock layers.
Any gap in age of rock between rock layers is called an uncomformity. An unconformity is the contact between two layers representing a gap in the geologic record, usually from the erosion of the layers which would normally be expected to appear.
A gap in an area's geologic history is called an unconformity. This represents a period of time where rock layers are missing due to erosion or non-deposition. Unconformities can help geologists understand the timing and duration of geological events.
Gaps in rock layers are called unconformities. Unconformities represent periods of time where deposition of sediment ceased and erosion occurred before deposition resumed, creating a gap in the geological record.
crack
When the surface of new rock layers meet a much older rock beneath them, it is called an unconformity. This represents a gap in the geologic record due to erosion or non-deposition between the older and younger rocks.
An unconformity is created when there is a gap in the rock record due to erosion or non-deposition of sediment. When sedimentation stops and then restarts, there is a period of time where the underlying rock is exposed to erosion, creating a gap in the sequence of rock layers. This gap represents missing geological time in the rock record.
A narrow gap or crack in a rock is commonly referred to as a fissure. This term describes a long, narrow opening in the rock where it has split or fractured. Fissures can vary in size and depth.
it is a natural rock formation from earth