because raindrops have small particles and coarse grained sedimentary rocks have big particles so it is easier for raindrop impressions to occur in fine grained sedimentary rocks
Vary fine sediments, such as mud, will crater when struck by raindrops. If the viscosity is not decreased by too much rainfall or influx of water, the raindrop impressions will be preserved when the mud dries. If subsequent sedimentation over the dried mud is rapid, the dried mud will not have time enough to dissolve by the influx of additional moisture. Thus the imprints may survive eventual lithification into rock. Coarser sediments would involve larger mineral and rock particle sizes and more pore space than finer, less porous sediments. The larger particles, and greater porosity would not be conducive to the creation of raindrop impressions or their preservation, as the drop would not cause a cratering of the impacted sediment, but rather pass around and through it.
Shale is a sedimentary rock formed from the compaction of fine-grained sediment such as mud or clay.
Breccia is a coarse-grained sedimentary rock that is composed of large, angular fragments.
Three types of sedimentary rock texture are clastic (made of broken fragments), crystalline (formed from the precipitation of minerals), and biogenic (composed of organic material such as shells or plant remains).
Sandstone is an example of a medium-grained clastic sedimentary rock. It is composed of sand-sized particles that are typically visible to the naked eye, giving it a medium-grained texture. Sandstone forms from the accumulation and cementation of sand grains.
Vary fine sediments, such as mud, will crater when struck by raindrops. If the viscosity is not decreased by too much rainfall or influx of water, the raindrop impressions will be preserved when the mud dries. If subsequent sedimentation over the dried mud is rapid, the dried mud will not have time enough to dissolve by the influx of additional moisture. Thus the imprints may survive eventual lithification into rock. Coarser sediments would involve larger mineral and rock particle sizes and more pore space than finer, less porous sediments. The larger particles, and greater porosity would not be conducive to the creation of raindrop impressions or their preservation, as the drop would not cause a cratering of the impacted sediment, but rather pass around and through it.
Vary fine sediments, such as mud, will crater when struck by raindrops. If the viscosity is not decreased by too much rainfall or influx of water, the raindrop impressions will be preserved when the mud dries. If subsequent sedimentation over the dried mud is rapid, the dried mud will not have time enough to dissolve by the influx of additional moisture. Thus the imprints may survive eventual lithification into rock. Coarser sediments would involve larger mineral and rock particle sizes and more pore space than finer, less porous sediments. The larger particles, and greater porosity would not be conducive to the creation of raindrop impressions or their preservation, as the drop would not cause a cratering of the impacted sediment, but rather pass around and through it.
Vary fine sediments, such as mud, will crater when struck by raindrops. If the viscosity is not decreased by too much rainfall or influx of water, the raindrop impressions will be preserved when the mud dries. If subsequent sedimentation over the dried mud is rapid, the dried mud will not have time enough to dissolve by the influx of additional moisture. Thus the imprints may survive eventual lithification into rock. Coarser sediments would involve larger mineral and rock particle sizes and more pore space than finer, less porous sediments. The larger particles, and greater porosity would not be conducive to the creation of raindrop impressions or their preservation, as the drop would not cause a cratering of the impacted sediment, but rather pass around and through it.
shale
sandstone
Shale is a sedimentary rock formed from the compaction of fine-grained sediment such as mud or clay.
Breccia is a coarse-grained sedimentary rock that is composed of large, angular fragments.
Three types of sedimentary rock texture are clastic (made of broken fragments), crystalline (formed from the precipitation of minerals), and biogenic (composed of organic material such as shells or plant remains).
Sandstone is an example of a medium-grained clastic sedimentary rock. It is composed of sand-sized particles that are typically visible to the naked eye, giving it a medium-grained texture. Sandstone forms from the accumulation and cementation of sand grains.
conglomerate
No, mudstone is a type of sedimentary rock formed from the compression and cementation of fine-grained mud and silt particles. Metamorphic rocks are formed from the alteration of pre-existing rocks due to high pressure, temperature, or chemical processes.
Shale.