yes.
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.
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.
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.
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.
Shale forms from the compaction of mud or clay sediments, often in quiet water environments such as lakes or deep ocean basins. These sediments are typically rich in fine particles such as clay minerals and organic matter, which bond together to create the layered structure of shale.
Quartzite
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.
Shale
no
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.
Shale
Because sandstone has wider particles than shale and this let's the water through.
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.
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.
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.
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.