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First it would change to Slate, but with increasing heat and pressure, it would eventually become Phyllite, then Schist, and finally Gneiss.

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What causes shale to change into slate?

Shale changes into slate through a process called metamorphism, which involves heat, pressure, and chemical changes. The heat and pressure cause the minerals in the shale to recrystallize into a denser, more compact form, resulting in the fine-grained texture and foliation characteristic of slate. The composition of the original shale, as well as the intensity and duration of the metamorphic conditions, influence the final characteristics of the slate.


Shale is a sedimentary rock that can be metamorphosed into slate by?

subjected to heat and pressure. The intense heat and pressure cause the shale's minerals to recrystallize, giving rise to the fine-grained texture and foliation characteristic of slate.


How can shale be turned into slate?

Shale can be turned into slate through metamorphism, which involves applying heat and pressure to the shale over time. This process causes the minerals in the shale to recrystallize and align, creating the distinct layers, smooth texture, and foliation characteristic of slate.


What is formed from shale exposed to great pressure?

Shale exposed to great pressure can form slate, a fine-grained metamorphic rock. The intense pressure and heat cause the clay minerals in the shale to recrystallize, resulting in a denser and more durable rock with distinct foliation.


What is slate formed by?

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.

Related Questions

Can heat and pressure change the sedimentary shale into slate?

No


Can heat and pressure change the sedimentary rock shale into slate?

No


What is shale after heat and pressure?

Slate is the metamorphic rock that forms from shale after it is exposed to heat and pressure for a llllloooooonnnnnnnggggg time.


Rocks formed from shale?

Shale can metamorphose through heat and pressure into slate.


What causes shale to change into slate?

Shale changes into slate through a process called metamorphism, which involves heat, pressure, and chemical changes. The heat and pressure cause the minerals in the shale to recrystallize into a denser, more compact form, resulting in the fine-grained texture and foliation characteristic of slate. The composition of the original shale, as well as the intensity and duration of the metamorphic conditions, influence the final characteristics of the slate.


Shale is a sedimentary rock that can be metamorphosed into slate by?

subjected to heat and pressure. The intense heat and pressure cause the shale's minerals to recrystallize, giving rise to the fine-grained texture and foliation characteristic of slate.


What does shale turn into when its expossed to heat and pressure?

High pressure can cause the formation of the metamorphic rock slate from the sedimentary rock shale.


How can shale be turned into slate?

Shale can be turned into slate through metamorphism, which involves applying heat and pressure to the shale over time. This process causes the minerals in the shale to recrystallize and align, creating the distinct layers, smooth texture, and foliation characteristic of slate.


What is the formation of slate?

when shale is subjected to heat and pressure, it can be metamorphosed into slate.


When shale is exposed to heat and pressure this metamorphic rock is formed?

gneiss


What is similarities between shale and slate?

Slate and shale have the same make-up. Slate is formed from sedimentary shale by pressure and heat. Wet shale has the same smell that wet slate has.


What sequence of change in rock type occurs as shale is subjected to increasing heat and pressure?

Shale undergoes metamorphism and transforms into slate, then phyllite, followed by schist, and eventually gneiss as heat and pressure increase. This progression represents a sequence of increasing metamorphic grade from low (slate) to high (gneiss) with changes in mineral composition and texture.