First of all, Gypsum is a mineral, and Rock Gypsum is a rock, don't get them confused. Second of all, no they aren't. Rock Gypsum is a sedimentary rock, and an alternate name for it is Alabaster.
Physical precipitation of gypsum due to the evaporation of seawater produces sedimentary rock called gypsum rock or rock gypsum.
Gypsum is an extrusive sedimentary rock formed from the evaporation of seawater.
Some sedimentary rock is formed this way; chemical sedimentary rock formed from evaporites, like rock salt, and rock gypsum.
Gypsum rock has a crystalline structure, typically forming in layers or beds within sedimentary rock deposits. It consists of calcium sulfate dihydrate, with a chemical formula of CaSO4·2H2O. The mineral gypsum has a soft texture and can be easily scratched with a fingernail.
sedimentary
Gypsum is actually a major rock forming mineral. Rock gypsum is a chemical sedimentary rock.
Physical precipitation of gypsum due to the evaporation of seawater produces sedimentary rock called gypsum rock or rock gypsum.
Gypsum is an extrusive sedimentary rock formed from the evaporation of seawater.
Rock salt, rock gypsum, and sometimes limestone.
yes and no because sedementary is a type of rock but it is not a rock like gypsum.
Rock gypsum is a sedimentary rock. These rocks can be transparent or opaque. Examples could be chalk and chalk boards.
Rock gypsum is a sedimentary rock. These rocks can be transparent or opaque. Examples could be chalk and chalk boards.
Rock salt and rock gypsum are common examples of a group of chemical sedimentary rocks called evaporities. When a sedimentary rock consists of angular, grave sized particles is breccia.
They are called chemical sedimentary rocks. Rock salt and rock gypsum are two examples.
Some sedimentary rock is formed this way; chemical sedimentary rock formed from evaporites, like rock salt, and rock gypsum.
Halite and Gypsum, they are called Evaporites and are both rocks and minerals
Gypsum is a mineral that was formed by layers of sediment , fine particles, that were deposited over a period of time, and then subjected to geologic forces.