Sedimentary rocks exist in curved and interrupted forms due to the processes of deposition, compaction, and lithification influenced by various environmental factors. During sedimentation, layers of sediments can be deposited in different orientations and under varying conditions, such as changes in water currents, wind patterns, or tectonic activity, leading to bending and folding. Additionally, erosion can remove sections of rock, creating interruptions in the layers. These phenomena reflect the dynamic Earth processes that shape sedimentary environments over time.
Detrital sedimentary rock. clastic sedimentary A+
That forms sedimentary rock.
Sedimentary rock
Clastic sedimentary rock forms when fragments of preexisting rocks are compacted or cemented together. Organic sedimentary rock forms from the remains of plants or animals. Chemical sedimentary rock forms when minerals precipitate from a solution or settle from a suspension.
Sedimentary rock forms from materials like sediment, minerals, and organic matter that settle and accumulate over time. These materials are compacted and cemented together to form sedimentary rocks such as sandstone, shale, and limestone.
It forms by
Clastic sedimentary rock forms when fragments of preexisting rocks are compacted or cemented together. Organic sedimentary rock forms from the remains of plants or animals. Chemical sedimentary rock forms when minerals precipitate from a solution or settle from a suspension.
That would be sedimentary rock, and (honorable mention) occasionally metamorphic rock.
Detrital sedimentary rock. clastic sedimentary A+
Detrital sedimentary rock. clastic sedimentary A+
Trapezus
A sphere has a total curved surface. A cylinder and a cone have a partial curved surface
sedimentary
sedimentary
Metamorphic and sedimentary
sandstone
Lithification