rocks and minerals Flashcards
Whats is GIS
- geogrpahic information systems
- store, analyze, and visulaize data for geographic positions on Earth’s surface
- a computer-based tool that examines spatial relationships, patterns, and trends in geogrpahy
what is a mineral
- a naturally occuring, soild inorganic substance with a specific chemical composition
- often forms in crystal lattice
- ex. quarts, ice
what is a rock
- and aggregate of minerals or non-minerals without a specific chemical composition
- no specific chemical formula
- classified based on certain parameters
- ex. schist with visible garnet crystals
general mineral info
- most important rock-forming minerals contain silicon and oxygen. this forms silicates
- 90% of minerals in Earth’s crust fall in 5 groups of silicates:
- quarts- silica
- feldspars
- pyroxene- Fe, Mg
- mica
- clay minerals (kaoliinite, montmorillonite)
- non-cilicate minerals: common on Earth’s surface; calcite and colomite
- ore minerals: magnetite, hematite, galena, sphalerite
how do we identify minerals
- colour
- streak
- luster
- harness (scratchability)
- cleavage
- fracture
- specific gravity
- magnetism
colour identifiication
- most noticeable
- least accurate
streak
- colour when mineral ground to a fine powder
- silicate minerals do no streak because they are stronger than the ceramic plate
- hematite streaks red/brown
luster
- reflection of light from mineral surface
- metallic
- or non-metallic
- ex. galena, spharelie, talc
hardness
- moh-harness scale (1-10)
- talc (very soft)- 1
- diamond- 10
- fingernail, copper penny, knife/glass plate, steel nail, masonary drill bit
cleavage
- ability of a mineral to break along preferred directions when struck
fracture
- surface along which a mineral breaks; not controlled by cleavage
- cannot have both fracture and cleavage, one or the other
specific gravity
- way to express density
- ratio of density of mineral to water
- water p=1
- magnetite has a specific gravity value of 5.2, meaning 1cm3 of magnetite will be 5.2 times as heavy as 1cm3 of water
magnetism
- some minerals are magnetic others are not
rock cycle
- change from one type to another with time
- KNOW DIAGRAM FOR EXAM IT WILL BE ON THERE
what is an igneous rock
- also called volcanic rocks
- form from solidified magma
- either at the Earth’s surface (extrusive) or underground/below Earth’s surface (intrustive)
ways igneous rocks are classified
- Texture
- mineralogy
texture for igneous rocks
- coarse grained igneous rocks cooled slowly beneath Earth’s surface allowing large crystals to form
- these rocks are INTRUSIVE and are called phaneritic
- can you see individual grains?
- fine grained igneous rocks cooled quickly on the Earth’s surface so large crystals did not have time to form
- these rocks are EXTRUSIVE and are called aphanitic
mineralogy
- colour of the rock often reflects the composition of the rock
- felsic rocks are light in colour, have high silica content and contain light-coloured minerals
- mafic rocks are dark in colour, have low silica content and contain dark-coloured minerals
sedimentary rocks
- form from sediment grains transported by water, ice, or air
- compacted, cemented- lithified
- clastic rocks (form from pre exisiting rocks from erosion and weathering)
- ex. conglomerate, sandstrone, shale (mudstone)
- clasts and matrix: clastic sedimentary rocks are made up of cemented particles (clasts or grains)
- often with matrix (finer-grained maerial) between the large grains
- chemical precipitates of bioclastic debris ex. limestone- fossil fragments, evaporites- halite
grain size sedientary rocks
- described using the udden-wentworth scale
- use a grain size card when looking at hand samples
grain size distribution
- sorting: organization according to grain size
- well sorted (same size)
- poorly sorted (variable sizes)
- can tell us distance from source (poorly indicates closer to sedimentary source)
grain shape
- very angular to well rounded
- angular means closer to source
metamorphic rocks
-metamorphism refers to changes to rocks that take place in the Earth’s interior
- the changes may be new textures, new mineral assemblages or both
- the new rocks is a metamorphic rocks
shale to slate to phyllie to schist to gneiss
sandsone to quartzite
limestone to marble
basalt to hornfels
texture for metamorphic rocks
- how minerals are alinged or bonded
- how they are oriented
- different than from sedimentary
- foliated: minerlas are alligned
- foliation is caused by differential stress which deforms objects into flattened forms
types of foliation
- slaty: nearly perfect, planar foliation with fine (mircoscopic) grains
- phyllitic: parallel, wavy foliation with a shiny/glossy lustre, fine grains
- schistose: parallel and subparallel foliation, medium to coarse grains
- gneissic: alternating light and dark layers, medium to coarse grains
- non foliated metamorphic rocks: rock name on basis of composition. ex. marble or quartzite
rock vs mineral
- a rock is naturally formed, consolidated material composed of grains of one or more minerals
- a mineral is a naturally occuring, inorganic, crystalline solid that has a definite chemical composition