The answer is sandstone.
Siltstone is a sedimentary rock, not an igneous one. It is composed primarily of silt-sized particles, which are finer than sand but coarser than clay. Siltstone typically forms from the compaction and cementation of silt particles, often in quiet water environments like lakes or floodplains. It is classified as a clastic sedimentary rock due to its composition and formation process.
Sandstone is a sedimentary rock classified as a clastic sedimentary rock. It is primarily composed of sand-sized mineral particles or rock fragments, typically quartz or feldspar, that have been compacted and cemented together over time.
Shale typically has a fine-grained texture, appearing smooth and often layered or fissile, allowing it to split easily into thin sheets. In contrast, conglomerate consists of larger, rounded clasts or pebbles embedded in a finer matrix, giving it a more coarse and variable texture. Sandstone, on the other hand, is composed primarily of sand-sized grains and has a more granular appearance, often with visible individual grains. Overall, shale is distinct due to its finer texture and layered structure compared to the coarser, more variable textures of conglomerate and sandstone.
Sedimentary rocks with a definite grain size include sandstone, which is composed of sand-sized grains, and conglomerate, which consists of larger, rounded clasts. Siltstone and claystone also exhibit specific grain sizes, with siltstone composed of silt-sized particles and claystone made up of even finer clay particles. These rocks are classified based on the size of their constituent grains, which helps in understanding their formation and depositional environments.
If the texture is coarser, then the surfaces will tend to "catch" more as they try to move. Coarser texture means more friction; finer texture means less.
Sandstone
The rock type finer than conglomerate but coarser than siltstone is sandstone. Sandstone is a sedimentary rock composed mainly of sand-sized grains, which are larger than the particles found in siltstone but smaller than the pebbles and cobbles in conglomerate.
Sandstone is a sedimentary rock classified as a clastic sedimentary rock. It is primarily composed of sand-sized mineral particles or rock fragments, typically quartz or feldspar, that have been compacted and cemented together over time.
It doesn't. The grain size effects the texture. If a rock has a small grain size, it will have a smooth texture. If the grain size is large, such as pebbles, the texture will be rough. For example, siltstone is one of the smoothest rocks because it contains silt particles, which are .0004cm to .006cm. Conglomerate though contains various particles including cobbles and boulders, which are from 10cm to 100cm.
the longer the soil partical the coarser it will be
Sandstone and siltstone are both sedimentary rocks formed from the accumulation of mineral grains through compaction and cementation. However, sandstone is predominantly composed of sand-sized grains, while siltstone contains finer silt-sized grains. Both rocks are commonly found in layers or beds and can exhibit a variety of colors and textures depending on their mineral composition.
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.
Shale typically has a fine-grained texture, appearing smooth and often layered or fissile, allowing it to split easily into thin sheets. In contrast, conglomerate consists of larger, rounded clasts or pebbles embedded in a finer matrix, giving it a more coarse and variable texture. Sandstone, on the other hand, is composed primarily of sand-sized grains and has a more granular appearance, often with visible individual grains. Overall, shale is distinct due to its finer texture and layered structure compared to the coarser, more variable textures of conglomerate and sandstone.
wheat flour is sifted, the finer atta is seperated, and what remains, the slightly coarser atta, is rava.
Finer particles will blend more perfectly. Coarser particles will make a less homogenous mixture.
If the texture is coarser, then the surfaces will tend to "catch" more as they try to move. Coarser texture means more friction; finer texture means less.
A conglomerate or a breccia. However, these rocks also have a finer-grained matrix.