Slaty cleavage is a result of stress and strain during the metamorphism process where the minerals that make up the slate become deformed and or re-crystallise with an orientation normal to the principle stress field. The fissile nature of shale is a result of the preferential alignment of clay minerals during the formation of the rock. This is because clay minerals are plate like and so form horizontal layers much like you would get if you stacked playing cards.
The cleavage of a shale rock refers to its tendency to break along flat, parallel planes due to its layered structure. This cleavage planes are a result of the alignment of clay minerals within the rock, allowing it to split easily along these planes. Cleavage in shale rocks can enhance its ability to split into thin sheets or slabs.
Shale is a clastic sedimentary rock. Which means that it is a rock made from sediments derived from other rock and organic matter that are compacted or cemented together. Shale is composed of clay or silt sized particles and exhibits fissility, a property which allows it to be split into thin sheets. Shale is formed from the deposition of these fine grained sediments in a relatively still environment such as the bottom of a lake or sea.
the metamorphic rock that is easily split is...A Mica, A Pumice and A Sulfur
Slate is formed from the metamorphism of shale or mudstone. This process involves intense heat and pressure which causes the shale to recrystallize into a fine-grained, foliated rock with excellent cleavage properties.
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.
The Shale is not a metamorphic rock it is a sedimentary rock.
the cleavage is Poor
The cleavage of a shale rock refers to its tendency to break along flat, parallel planes due to its layered structure. This cleavage planes are a result of the alignment of clay minerals within the rock, allowing it to split easily along these planes. Cleavage in shale rocks can enhance its ability to split into thin sheets or slabs.
Shale is a fine-grained sedimentary rock composed of clay minerals and other debris. It typically forms in layers, known as laminae, which give it its characteristic fissility. Shale is typically dark in color and can contain varying amounts of organic matter, making it an important source rock for hydrocarbons.
Shale rocks are composed of fine-grained sedimentary particles, mainly clay minerals such as illite, kaolinite, and chlorite. They are known for their fissility, or tendency to split into thin layers along bedding planes. Shale rocks are commonly found in sedimentary basins and are an important source of natural gas and oil.
u answer is................ i think it is............................ metamorphosed shale with very flat, well defined cleavage planes THANK U FOR UR TIME from: Shilo Kim Johnson
Halite and Calcite. Halite has what is known as cubiccleavage, where there is cleavage in three directions at 90 degree angles. Calcite has what is known as rhombohedral cleavage, where there is cleavage in three directions but at 120 and 60 degree angles.
It is a surname of English origin (Norfolk).
Shale is a clastic sedimentary rock. Which means that it is a rock made from sediments derived from other rock and organic matter that are compacted or cemented together. Shale is composed of clay or silt sized particles and exhibits fissility, a property which allows it to be split into thin sheets. Shale is formed from the deposition of these fine grained sediments in a relatively still environment such as the bottom of a lake or sea.
the metamorphic rock that is easily split is...A Mica, A Pumice and A Sulfur
Slate is formed from the metamorphism of shale or mudstone. This process involves intense heat and pressure which causes the shale to recrystallize into a fine-grained, foliated rock with excellent cleavage properties.
With increases of heat and pressure deep underground on shale, chlorite and mica minerals form and line up along basal cleavages, imparting the new rock slate with "slatey" cleavage. Slately cleavage is a characteristic of rock that can be broken into thin sheets with smooth flat faces. Visible on these smooth flat faces is a somewhat noticeable sheen from light reflection. This occurs as the light is bounced off the aligned cleavage faces of the minerals contained in the slate.