sediments
The most noticeable characteristic of sedimentary rock is its layered appearance, which is known as "bedding." These layers are formed over time as different sediment deposits accumulate and are compressed together.
rocky
fault-block mountain.
Igneous rocks can disturb sedimentary rock layers and formations by their movement during ascent through such layer. when they make contact with this sedimentary rocks they could result to folding and/or metamorphism.
Strata can be found in sedimentary rocks, which form in layers over time as sediments accumulate and compact. Igneous rocks, which form from molten magma cooling and solidifying, do not typically have distinct layers or strata.
The presence of layers is the universal feature of all sedimentary rock.
Stratification. The existence of layers.
The most noticeable characteristic of sedimentary rock is its layered appearance, which is known as "bedding." These layers are formed over time as different sediment deposits accumulate and are compressed together.
Sedimentary rocks are often deposited in layers as strata. The feature that tells how a sedimentary rock is layered is called the bedding.
rocky
Sedimentary rocks are often deposited in layers as strata. The feature that tells how a sedimentary rock is layered is called the bedding.
Cross-bedding refers to inclined layers in sedimentary rock that were formed as a result of wind or water driven ripples or dunes in the original depositional environment.
Sedimentary rock layers. your welcome
An antiform is a topographic feature which is composed of sedimentary layers in a convex formation, or an artform which defies the usual convention of artforms.
fault-block mountain.
Sedimentary rock, like limestone, is formed in layers.
sedimentary rock