Siltstone can be formed from the eroded and transported particles of any rock type.
siltstone
Siltstone is a type of sedimentary rock composed mainly of silt-sized particles. These particles are cemented together over time to form a solid rock. Siltstone has a fine-grained texture and is commonly found in geological formations where sediments have accumulated.
Silt particles cemented together form a sedimentary rock known as siltstone. Siltstone is composed mainly of silt-sized particles compacted and cemented over time. It has a fine-grained texture and is commonly found in layers or beds in sedimentary rock formations.
Sedimentary rocks
Sometimes, but not always!
Siltstone is gritty to the touch. It has the texture of a very fine-grained sandpaper
Siltstone forms from the accumulation of fine particles, like silt, in a depositional environment such as river deltas, floodplains, lakes, and shallow marine environments. These particles are compacted and cemented together over time to create the sedimentary rock siltstone.
Limestone and siltstone
Siltstone.
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.
Siltstone is a sedimentary rock composed of cemented silt-sized particles of quartz and feldspar, primarily.
Siltstone is typically found in areas where fine-grained sediment has undergone compaction and cementation. It often forms in river and lake environments where silt-sized particles settle out of water and accumulate over time. Siltstone can also be found in marine settings and as part of sedimentary rock formations.