Hope this information will clear your doubts about the topic.
Limestone is changed into marble give reason.
It is about 4 km.
Because marble is a fairly soft material only a three on the mohs hardness scale it is easy to cut and carve.
With continued metamorphism these crystal seeds grow while any clay deposits in the limestone transform into silicate structures such as mica.
This metamorphic process causes a complete recrystallization of the original rock into an interlocking mosaic of.
Sedimentary rocks are formed from sediments.
It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is.
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These sediments are transported and deposited by wind water etc.
When the heat and pressure hits the limestone calcite seed crystals form.
We cannot go to the centre of the earth.
When it is subjected to conditions of extreme heat and pressure it gets converted into marble which is a metamorphic rock.
These loose sediments are compressed and hardened to form layers of rocks known as sedimentary rocks.
Since the temperature and pressure increase enormously as we go deeper and deeper inside the earth we cannot go to the centre of the earth.
Give reasons why limestone is changed into marble.
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Limestone is changed into marble.
Marble is a metamorphic rock that forms when limestone is subjected to great heat and pressure.
Inside our earth ncert solution give reasons.
Ii rocks break down into small fragments known as sediments.
Because of extreme compression and hardening of the particles of sediment which are deposited by wind.
Limestone is an example of a sedimentary rock.
Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.
Limestone change into marble when a great heat and pressure come from the under of the earth change into marble.
Marble is a metamorphic rock resulting from regional or rarely contact metamorphism of sedimentary carbonate rocks either limestone or dolostone.
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Iii limestone is changed into marble as a result of metamorphism under great heat and pressure.
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