Copyright: INTRODUCTION TO MINERALOGY, WIILIAM D. NESSE, 2nd Edition
Introduction
The term minerals
is used in a variety of ways:
In economic: any valuable material extracted from the earth like coal, oil, sand, gravel, iron ore, & groundwater
In nutritionists: any of the chemical compounds or elements that are important for health
common usage: anything that is neither animal nor vegetable
In geoligy: naturally occurring with crystalline solid
Some definition require inorganic material, but some mineral have organic material called bio mineral
Mineralogy: study of minerals
naturally occurring
formed without benefit of human action in natural environment
synthetic mineral: crystalline solid produce in laboratory (It’s not mineral Because it’s not naturally occurring)
crystalline
atom comprise crystalline material arranged & bonded in regular & repeating long-rang pattern
amorphous: Solid like glass & opal lacking long-range order
Mineraloids: mineral-like, materials that lack long-range crystalline structure, include amorphous solid such as Opal & Glasses
Opal SiO₂.H₂O: consist silica gel arrange in small spherical masses
Any crystalline structure is solid material, but not every solid material have crystalline structure
Metamict: applied to disrupted structures, & once structure becomes metamict then it’s mineraloid
Composition & Properties
As consequence of being crystalline solid, minerals have definite & not necessarily fixed chemical composition
– Ex. Quartz SiO₂
composition of many mineral species may vary within limits
– Ex. olivine: may rich in iron Fe₂SiO₄ or magnesium Mg₂SiO₄, or intermediate composition
different sample of mineral may have different compositions but variability is limited, Because minerals are crystalline & have definite chemical composition & definite physical properties
– في الوحدات القادمة سنعلم ان السبب هو احلال العناصر
physical properties may vary within limits because they controlled by variation in chemical properties
bio mineral “in general”
bio minerals: Minerals constitute integral part of biologic structures & processes
Calcite & Aragonite (both CaCO₃): form shell & major component of limestone layers
Apatite: makes teeth & bones
Bacteria are integral part of geochemical processes at or near surface & influence at many minerals
pyrite FeS₂: found in shale & coal, & reduced by action of sulfate-reducing bacteria
Geomicrobiology: study of interaction of microbes & geologic processes
biologic processes : affect surface chemical environment & therefore types of distribution of minerals found
meteorite impacts
Pseu-dotachylite: Frictional melts produced in fault zones in response to intense shearing
If meteorite impacts are large enough, release high energy to melt rocks that they strike producing impact melt
impact melt ejected from impact crater
Tektite: Small mass of glass, interpreted to samples of now-solidified
lightning strike may heat soil or rock sufficiently to melt some of it & produce fulgurite
Burring coal beds generate heat to fuse surrounding rook (forming scoriaceous or slag-like glasses referred to as ash glass or clinker)
MINERAL NOMENCLATURE
Mineral Species: mineral distinguished from other minerals by combination of composition & structure
Mineral Variety: distinguished by differences in color, habit (shape)… atc
Mineral Series: is 2 or more minerals among there range of composition (Ex. Plagioclase)
Mineral Group: set of minerals with same structure & different compositions
Mineral Crystal: piece of mineral bounded by regular crystal faces produced as crystal grew, Like fracture, & cleavage
Commission on New Minerals Nomenclature & Classification of International Mineralogical Association