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It depends on: - the strength of the acid - concentration of the acid - temperature of the solution - stirring of the solution - granulation of the lime
Chalk would weather fastest, followed by limestone.
A humid climate would weather mechanics quickly. Also, in humid climates (i.e. Africa) there is also rain season which may help to weather mechanics even faster.
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Quartz
fine grained rock will weaher faster thatn the course grained rock
Fine grained rock exhibits a non-visible or nearly non-visible crystalline structure on a fractured surface. On the opposite end, a coarse grained rock exhibits mineral crystals of the rock's constituents on a fractured surface. The larger the crystals, the coarser grained is the rock. Basalt would be an example of a fine grained rock. Granite would be an example of a coarse grained rock.
The period of time involved in the rock cycle which would involve the transformation of a coarse grained rock into weathered, eroded, transported, deposited, and cemented fine-grained sedimentary particles would vary greatly. Suffice it to say the entire process would take many thousands-to-millions of years.
Visible crystals or grains would be referred to as a coarse grained texture.
Lava slowly flowing out of a fracture in the Earth's surface :)
Visible crystals or grains would be referred to as a coarse grained texture.
Methods of formation. If crystalline (igneous or metamorphic) they would most likely have had differing rates of cooling. If sedimentary, they would most likely have had differing depositional environments (higher energy for larger grain sizes).
Olivine would weather faster than quartz
Slow cooling in the upper mantle
Slow cooling in the upper mantle
Slow cooling in the upper mantle
It depends on: - the strength of the acid - concentration of the acid - temperature of the solution - stirring of the solution - granulation of the lime