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Which is most resistant to water erosion quartzite shale or sandstone?

Quartzite


Does Shale absorb water?

Shale is a type of sedimentary rock composed of fine-grained sediment particles, including clay and silt. While shale is porous and can contain water within its pore spaces, it does not absorb water like a sponge. Instead, water can flow through the interconnected pore network in shale.


What is that stone which is not dip into water?

Shale


Does a shale rock float in water?

no


Can a shale rock float?

No, shale rock is denser than water, so it will sink in water. It is composed of fine-grained minerals such as clay, which typically have a higher density than water.


What metamorphic rock is water proof?

Shale


Why can water pass easily through sandstone but not shale?

Because sandstone has wider particles than shale and this let's the water through.


Where is black shale found?

Black shale is a very thinly bedded shale rich in sulfides such as pyrite. It is commonly found in anoxic, reducing environments, such as in stagnant water columns.


How does water erode shale?

Water erodes shale primarily through a combination of chemical and physical processes. As water flows over shale, it can dissolve minerals within the rock, weakening its structure. Additionally, the mechanical action of flowing water can dislodge small particles, gradually wearing away the shale layers. Over time, this continuous action leads to the formation of rills, gullies, and other erosional features.


Rock formed when high concentrations crystallize in water?

Shale


What is the origin of shale?

Shale is a type of sedimentary rock that forms from the gradual accumulation of mud, clay, and silt particles at the bottom of bodies of water, such as oceans or lakes. Over time, these particles become compacted and cemented together to form the dense, fine-grained rock known as shale.


Is a Shale an aquifer?

Shale can act as an aquifer, but it is not as permeable as other types of rock like sandstone or limestone. Shale can store and transmit water to a certain extent, but its low permeability usually limits its ability to serve as a primary source of water for wells and springs.