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Marble is shaped when limestone is exposed to extreme warmth and pressure. Marble is regularly not foliated, in spite of the fact that there are special cases.
Complete Answer:
Marble is a sedimentary rock made out of recrystallized carbonate minerals, most normally calcite or dolomite. Marble is commonly not foliated, in spite of the fact that there are exemptions. In topography, the term marble alludes to transformed limestone, yet its utilization in stonemasonry all the more comprehensively incorporates metamorphosed limestone. Marble is normally utilized for design and as a structural material.
"Marble" gets from the Ancient Greek μάρμαρον (mármaron), "glasslike rock, sparkling stone", maybe from the action word μαρμαίρω (marmaírō), "to streak, shimmer, gleam"; R. S. P. Beekes has proposed that a "Pre-Greek cause is probable". Marble is a stone coming about because of the transformation of sedimentary carbonate rocks, most usually limestone or dolomite rock. Change causes variable recrystallization of the primary carbonate mineral grains. The ensuing marble rock is normally made out of an interlocking mosaic of carbonate diamonds. Essential sedimentary surfaces and structures of the first carbonate rock (protolith) have ordinarily been altered or devastated
This stem is additionally the precursor of the English word "marmoreal", signifying "marble-like." While the English expression "marble" looks like the French marble, most other European dialects (with words like "marmoreal") all the more intently take after the first Ancient Greek.
Note:
As the most loved model for Greek and Roman artists and engineers (see old-style form), marble has become a social image of custom and refined taste. It’s incredibly fluctuating and brilliant examples make it a most loved improving material, and it is regularly imitated in foundation designs for PC shows, and so forth.
Marble is shaped when limestone is exposed to extreme warmth and pressure. Marble is regularly not foliated, in spite of the fact that there are special cases.
Complete Answer:
Marble is a sedimentary rock made out of recrystallized carbonate minerals, most normally calcite or dolomite. Marble is commonly not foliated, in spite of the fact that there are exemptions. In topography, the term marble alludes to transformed limestone, yet its utilization in stonemasonry all the more comprehensively incorporates metamorphosed limestone. Marble is normally utilized for design and as a structural material.
"Marble" gets from the Ancient Greek μάρμαρον (mármaron), "glasslike rock, sparkling stone", maybe from the action word μαρμαίρω (marmaírō), "to streak, shimmer, gleam"; R. S. P. Beekes has proposed that a "Pre-Greek cause is probable". Marble is a stone coming about because of the transformation of sedimentary carbonate rocks, most usually limestone or dolomite rock. Change causes variable recrystallization of the primary carbonate mineral grains. The ensuing marble rock is normally made out of an interlocking mosaic of carbonate diamonds. Essential sedimentary surfaces and structures of the first carbonate rock (protolith) have ordinarily been altered or devastated
This stem is additionally the precursor of the English word "marmoreal", signifying "marble-like." While the English expression "marble" looks like the French marble, most other European dialects (with words like "marmoreal") all the more intently take after the first Ancient Greek.
Note:
As the most loved model for Greek and Roman artists and engineers (see old-style form), marble has become a social image of custom and refined taste. It’s incredibly fluctuating and brilliant examples make it a most loved improving material, and it is regularly imitated in foundation designs for PC shows, and so forth.
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