Quartz crystals range in size from cryptocrystalline (difficulty in observing even with microscopes) to gigantic. The largest individual quartz crystal recorded weighed more than 96,000 pounds and was roughly 20 feet in length.
Quartz crystals can be from cryptocrystalline (difficulty in observing even with microscopes) to gigantic. The largest quartz crystal recorded weighted more than 96,000 pounds and was roughly 20 feet in length.
The crystal size would refer to the dimensions of the individual mineral grains that comprise the rock. Some rock is composed of large crystal grains, some from small crystal grains, and some from a combination of various crystal grain sizes.
a crystal can get large depending on how much it grows
There is no real upper limit on the size a crystal can be. Some are HUGE!
The size of the crystal relates to how long the crystals were forming. For example crystals that cooled slowly are larger than those cooling faster.
the crystal size of its minerals
the crystal size of its minerals
The particle size (grain size--crystal size) in igneous rock is largely dependent on the amount of time spent cooling and solidifying from molten rock. If cooled quickly, crystals will have little time to grow. Slow cooling allows time for larger crystal growth.
that means like when somthing is in a own properties
the size of crystals in extrusive roks
texture
texture
it is metamorphic rock
What is the effect of location on crystal size? Label the location of intrusive and extrusive igneous rocks on the diagram below. Then, illustrate the crystal size of the rock formed at that location in the appropriate callout circles.
crystal size
It can be any size. The only specific factor of the intrusive rock is that is took a very long time to cool.
Grain refers to particle or crystal size in rock.
When it is broken down into an individual mineral grain or crystal, in which case it is a mineral.
please anyone else can answer this question I'm in hurry pls.
Limestone is a fine grained sedimentary rock.
The size of the crystal relates to how long the crystals were forming. For example crystals that cooled slowly are larger than those cooling faster.