An sedimentary enviorment is when all the rain rains in a puddle and all the rocks settle and a sedimentary enviorment develops/forms. This is my thinking/opinion.
Evaporites are sedimentary rocks formed when mineral solutions evaporate, leaving behind salts and minerals that precipitate and accumulate. Common examples of evaporites include rock salt, gypsum, and halite.
A 'high energy' depositional environment is characterized by strong currents, waves, or wind that have the ability to transport and deposit large particles quickly. These environments are typically found near coastlines, river deltas, or areas affected by storms, where the energy of the water or wind is sufficient to move sediments and create deposits.
Bedding or stratification: Layers of sediment that are typically horizontal and represent different depositional events. Cross-bedding: Inclined layers within sedimentary rocks that are formed by the migration of sediment in a current. Ripple marks: Small-scale features on the surface of sedimentary rocks caused by the action of water or wind. Graded bedding: Layers with gradually changing grain sizes, typically indicating a decrease in the energy of the depositional environment. Concretions: Rounded masses of mineral matter that are often found in sedimentary rocks, forming within the rock after its initial formation.
An area of deposition is a location where sediment is deposited by natural forces like water, wind, or ice. This can include river deltas, beaches, and glacial moraines. Over time, these deposits can build up and create new landforms.
Depositional environments are specific locations where sediment is deposited and accumulated, leading to the formation of sedimentary rocks. These environments can include riverbeds, shorelines, deltas, and ocean floors. They provide clues about the conditions under which the sediments were initially deposited.
Sedimentary depositional environment
depositional environments is the place or setting in which sediments is deposited. oceans, rivers, deltas, and beaches are all common depositional. each of the depositional environment has different characteristics that create specific structure in sedimentary rock.
A continental depositional environment is a geological setting on land where sediments accumulate and form sedimentary rocks. Examples include river, lake, desert, and glacial environments. These environments are characterized by unique sedimentary structures and features that reflect the specific conditions under which the sediments were deposited.
Bedding planes in sedimentary rocks indicate the separate layers or strata in which the sediment has been deposited over time. These planes can provide important information about the environment in which the rock was formed, including factors like sedimentation rate, depositional environment, and past geological events.
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.
A swamp
carbonate shelf
The deep ocean floor and submarine sand reefs are all made up of limestone environment. Limestone is a sedimentary type of rock that can be found in many places. It falls to the ocean floor when tides rise and fall.
I attached a picture with the answers on it
Evaporites are sedimentary rocks formed when mineral solutions evaporate, leaving behind salts and minerals that precipitate and accumulate. Common examples of evaporites include rock salt, gypsum, and halite.
A 'high energy' depositional environment is characterized by strong currents, waves, or wind that have the ability to transport and deposit large particles quickly. These environments are typically found near coastlines, river deltas, or areas affected by storms, where the energy of the water or wind is sufficient to move sediments and create deposits.
Answer Moderately sorted and fossiliferous would indicate perhaps a continental shelf depositional area.