Gypsum (hydrous calcium sulphate) is an evaporite mineral, which is to say that it is formed when a body of water rich in dissolved calcium sulphate either cools, or is concentrated by evaporation, to the point where the calcium sulphate precipates as a solid.
Gypsum is found in extensive, often thick strata where seas or lakes have evaporated. Less commonly it is found as a deposit in volcanic springs, or as veins or a cementing material in other rocks where it has precipitated from calcium-suphlate-rich groundwater in voids, cracks, and the interstices between grains.
The mineral composition and texture of the rock are most important in determining how a rock was formed. These factors provide clues about the conditions under which the rock formed, such as temperature, pressure, and the presence of fluids. By analyzing these characteristics, geologists can infer the rock's origin and history.
The rock was most likely formed through the process of sedimentation, where layers of sediment accumulated over time and eventually turned into rock through compaction and cementation. The fossil seashells in the rock suggest that the area was once covered by a sea or ocean where these organisms lived and were preserved in the sediment as it solidified into rock.
Evaporites are rock units that are most likely formed from chemical precipitates. These rocks are formed when minerals precipitate out of solution as water evaporates, leaving behind minerals like halite or gypsum.
Conglomerate rock is most likely formed from pebble-sized sediment deposited in shallow water at an ocean shoreline. As the pebbles accumulate, they cement together to form the rock.
Sedimentary rock can be formed from lithified sediments.
The mineral composition and texture of the rock are most important in determining how a rock was formed. These factors provide clues about the conditions under which the rock formed, such as temperature, pressure, and the presence of fluids. By analyzing these characteristics, geologists can infer the rock's origin and history.
Composition and texture
Clastic rock
they were formed by underwater volcanoes
That would be the rock basalt.
sansandrease
limestone
The rock was most likely formed through the process of sedimentation, where layers of sediment accumulated over time and eventually turned into rock through compaction and cementation. The fossil seashells in the rock suggest that the area was once covered by a sea or ocean where these organisms lived and were preserved in the sediment as it solidified into rock.
Rock was formed when the earth was made.
The rock formed from molten rock is called igneous rock. It is formed when magma cools and solidifies either underground as intrusive rock or on the Earth's surface as extrusive rock.
A rock that contains fossil seashells was most likely formed as a result of sedimentation.
The most often occurring metamorphic rock types are Dwayne the rock Johnson, Rockey, and pet rock.