Silt a particle slightly is larger than clay. Also, hence the name.
the smallest particles of sediment are found in clay.
Mudstone, claystone, and siltstone.
The strongest and hardest between marble, dolerite, clay, and siltstone is marble. It is considered to be a mineral that is very hard and strong. It can hold up better to the elements than the other three.
silt
Siltstone is a sedimentary rock which has a grain size in the silt range, finer than sandstone and coarser than claystones.DescriptionSiltstone is a clastic sedimentary rock. As its name implies, it is primarily composed (greater than 2/3) of silt sized particles, defined as grains 1/16 - 1/256 mm or 4 to 8 on the Krumbein phi (φ) scale. Siltstones differ significantly from sandstones due to their smaller pores and higher propensity for containing a significant clay fraction. Although often mistaken as a shale, siltstone lacks the fissility and laminations which are typical of shale. Siltstones may contain concretions. Unless the siltstone is fairly shaly, stratification is likely to be obscure and it tends to weather at oblique angles unrelated to bedding. Mudstone or shale are rocks that contain mud, which is material that has a range of silt and clay. Siltstone is differentiated by having a majority silt, not clay.
Clay particles have a permanent negative charge.
The mineral component of soil texture is comprised of three types: sand is the largest, silt is next, and clay is the smallest. Soil also contains varying amounts of organic matter, flora and fauna.
Siltstone is formed when silt-sized sediments are turned into rock. This happens when the silt sized sediments are compacted
Clay particles are of colloidal dimension i.e. 1 to 2 microns .
No, silt contains quartz and feldspar and is inorganic
Clay is very made up of very small tightly fitting particles and is non-porous and does not absorb water, which is why it is used to make pottery and ceramics. Sand is larger particles and can absorb large quantities of water.
The size of rock particles are important to soil structure because the larger particles of sand allow rainwater to drain quickly through the soil, while the smaller particles of clay prevent rapid drainage.