Stonehenge is not a natural formation, it was built by people.
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
cleansing of the the blood
melting and crystallization
The three basic types of unconformities:angular unconformities, disconformities, and nonconformities.
Cementing is not a process involved in the formation of sedimentary rock.
Orogenic processes refer to the geological processes involved in the formation of mountain ranges through the collision and convergence of tectonic plates. These processes can include folding, faulting, metamorphism, and volcanic activity. Orogenic events can result in the uplift of rocks and the formation of large mountain chains.
Coal is formed from the remains of plants that lived millions of years ago. The key processes involved in its formation include the accumulation of plant material in swamps, burial under layers of sediment, and the slow transformation of the plant material into coal through heat and pressure over time.
Chert is formed through the accumulation of silica-rich sediments, such as microcrystalline quartz, in marine environments. The key processes involved in its formation include the deposition of silica from organisms like diatoms and sponges, as well as the chemical precipitation of silica from seawater. Over time, these processes lead to the compacting and hardening of the silica-rich sediments into chert rock.
Sedimentory rocks form in several stages, which are: weathering, errosion, sedimentation, cementation and at the end lithification.
The three basic steps are erosion (weathering), transport (carrying silt), and deposition (carried load settles out).