No. It is not uncommon for the layers to be shifted out of a horizontal position.
The relative age of the fault is younger than the sedimentary rock layers it cuts across. The fault must have formed after the deposition of the sedimentary rock layers, as it disrupts them.
Horizontal layers of rocks are rock layers that are parallel to the Earth's surface. These layers are typically formed over time through sedimentary processes, such as deposition of sediment in water or air. The horizontal orientation of these layers indicates the original horizontal position in which they were deposited.
Sedimentary rock layers. your welcome
A disconformity exists between parallel layers of sedimentary rock. This is when there is a gap in the rock record represented by a horizontal surface separating younger strata from the older ones.
Horizontal layers in sedimentary rocks are formed from the accumulation of sediment particles over time, usually in a fairly uniform manner. In contrast, bands in metamorphic rocks are created from the process of intense heat and pressure altering the original rock's mineral composition, resulting in distinct layers of different minerals. These bands are not necessarily deposited in a uniform manner like sedimentary rock layers.
A sill is a horizontal intrusive igneous body that forms between sedimentary rock layers. Sills are formed when magma intrudes parallel to the layering of the surrounding rocks and solidifies underground.
The largest grains will always be deposited first so they will be at the bottom of the beds because they could not form natrually any other way.
Sedimentary rock, like limestone, is formed in layers.
Sedimentary rocks are types of rock that are formed by the deposit of material at the Earth's surface and within bodies of water. The horizontal layering happens because it has forms with the passing of time over thousands if not millions of years.
sedimentary rock
Sedimentary rock, such as sandstone or shale, often has visible flat layers called strata that form from the accumulation and compression of sediments over time. These layers can be easily distinguished in sedimentary rocks due to their distinct horizontal orientation.
That would be sedimentary rock, and (honorable mention) occasionally metamorphic rock.