hydrates
Terrigenous
hydrates
hydrates
mid ocean ridges
hydrates
Terrigenous
hydrates
hydrates
hydrates
mid ocean ridges
hydrates
Detrital sediment consists primarily of mineral grains that were eroded from rocks on land. These mineral grains are transported by wind, water, or ice and eventually settle and accumulate to form detrital sedimentary rocks, such as sandstone or shale.
mid ocean ridges
hydrates
Rock gypsum is formed by precipitation from saturated solutions that are composed primarily of dissolved gypsum. In this case, there is no true sediment, only the solution containing the dissolved mineral that was originally present in weathered and eroded rock.
Rock salt is formed from the evaporation of saturated solutions that are composed primarily of dissolved halite. In this case, there is no true sediment, only the solution containing the dissolved mineral that was originally present in weathered and eroded rock.
hydrates