Mica is made up of sheets of silicate
Muscovite generally displays a micaceous crystal habit, of thin flexible sheets.
Foliation in rocks refers to the process being split into thin sheets. It is caused by intense pressure that shapes rocks to align in particular directions.
The cleavage of mica is perfect. Sometimes it has parallel parting. The cleavage laminae is flexible and elastic. The thin translucent sheets allow geologists to view the metamorphosis.
A Huron longhouse was usually made from white birch or alder trees that were small enough to bend, rope that had been made by braiding together thin strips of bark, and sheets of bark to cover the frame.
. The commercially important micas are muscovite and phlogopite, which are used in a variety of applications. Mica's value is based on several of its unique physical properties. The crystalline structure of mica forms layers that can be split or delaminated into thin sheets usually causing foliation in rocks. These sheets are chemically inert, dielectric, elastic, flexible, hydrophilic, insulating, lightweight, platy, reflective, refractive, resilient, and range in opacity from transparent to opaque
Shale and slate can be cleaved into thin sheets of rock.
yes because it splits to thin elastic sheets
Generally in books of thin sheets.
cleavage
cleavage
Muscovite mica has perfect cleavage in one direction. It splits into thin sheets.
Muscovite mica has perfect cleavage in one direction. It splits into thin sheets.
The mica group of minerals (phyllosilicates) fits this description.
Slate which is a type of stone is used for the roof tiles instead of shingles. It splits in thin sheets and is nailed to the roof the same as regular asphalt shingles.
Slate is a hard, dark grey rock which splits into thin sheets (along a pronounced and dominant cleavage), which makes it very suitable for roofing material.
Slate is formed by heat and pressure on shale or mud stone. It splits into perfectly cleaved, broad thin sheets. It is a sedimentary rock made of volcanic ash.
Slate is formed by heat and pressure on shale or mud stone. It splits into perfectly cleaved, broad thin sheets. It is a sedimentary rock made of volcanic ash.