Chemical (or non-clastic) sedimentary rock.
A "Desert Rose" is not a living organism, it is a formation of gypsum crystals that form in desert regions where there are mineral(salt) rich ground waters evaporating near the ground surface.
Conglomerate consists of cemented pebbles of various sizes.
At foot-slopes of rocks, around desert regions, and at river banks/mouth.
Sedimentary rocks like rock gypsum and rock salt are typically found in arid environments, such as desert regions, or in areas that were once covered by shallow seas or lakes. They often form in evaporite deposits, where minerals precipitate from evaporating saline water. Common locations include salt flats, playas, and ancient seabeds, with notable examples found in places like the Great Salt Lake in Utah and the Permian Basin in Texas.
By evaporating the water out, which precipitates the sugar back into its crystalline form.
Examples of biochemical sedimentary rocks include limestone, which forms from the accumulation of shells and coral fragments, and chert, which is formed from the silica-rich remains of marine organisms. Evaporites are sedimentary rocks that form from the precipitation of minerals from evaporating water bodies, such as rock salt (halite) and gypsum, which are common examples.
If the original rock is eroded or broken away and then returned to sedimentary-forming conditions, it will form another sedimentary.
Sedimentary rocks form from a few different things. Sedimentary rocks form from sediment is deposited out of air, ice, wind and gravity.
Sediment with a diameter of 0.0002 cm would likely form siltstone, a fine-grained sedimentary rock. Siltstones are composed of particles smaller than sand but larger than clay, and they form when silt-sized particles compact and cement together over time.
Sediments of 0.0002 cm in diameter would likely form siltstone, a type of sedimentary rock composed primarily of silt-sized particles. Siltstone has a fine-grained texture, as silt particles are smaller than sand but larger than clay.
You might expect to find chemical sedimentary rocks in environments where minerals precipitate out of solution, such as in evaporating seas, hot springs, or caves. These rocks form when minerals are dissolved in water and then crystallize out as the water evaporates or mineral saturation levels change.
All rocks can form from sedimentary because the rock cycle is endless.