Rocks Flashcards
(36 cards)
3 groups of rocks
- igneous (hot rocks/fire)
- sedimentary
- metamorphic
Rocks
-Made up of minerals
-Makes up the geosphere
Most rocks are made of several minerals but some are monomineralic (one mineral)
Igneous
Rocks formed by crystallization of magma/lava during cooling
Sedimentary
Formed at or near earth’s surface from sediment that may include mineral or rock fragments, organic fragments (sandstone), by precipitation from water (limestone)
Metamorphic
Formed from igneous, sedimentary or previously metamorphosed rocks by heating and/or increase in pressure during collision of tectonic plates or magma intrusion
Major environment issues associated with igneous activity
- volcanic hazards
- sources of many ore deposits
- driving energy and nutrients for some important ecologic systems
- driving energy for geothermal systems
- building materials
Igneous rocks
(intrusive vs extrusive)
(plutonic vs volcanic)
-lava flow (volcanic/extrusive)
-magma chamber (plutonic/intrusive)
Plutonic vs volcanic:
-plutonic (slowly cooled)
-volcanic (rapidly cooled)
Igneous rock
Ferromagnesian (dark color)
- olivine
- pyroxene
- amphibole
- biotite
Igneous rock
Felsic (light color)
- plagioclase feldspar
- orthoclase feldspar
- Quartz
- muscovite
Things that control igneous rock composition
- composition of the source
- magnetic differentiation
Provenance of igneous rock composition
- mantle is made of peridotite
- mantle source -> basalt, andesite, dacite (and their plutonic equivalents: gabbro, diorite, granddiorite)
- continental crust source -> rhyolite (and it’s plutonic equivalent: granite)
Magmatic differentiation
-process by which a homogenous magma segregates into different rock types
Magmatic differentiation: sequential crystallization of minerals permits their separation
High density minerals will sink inside a magma chamber, low density minerals will float inside a magma chamber
Fractional crystallization
The separation of minerals, it is the most common type if magmatic differentiation
Making of sedimentary rocks
1) weathering
- mechanical (erosion, breaking rocks apart)
- chemical (chemical reactions)
2) sedimentation (transport and deposition)
3) Lithification
Weathering
Is the response of rocks to new conditions at or near Earth’s surface
-for example, minerals in lava that crystallized at 1000 degrees Celsius are not very stable at surface conditions
Agents of mechanical weathering (erosion)
- running water
- wind
- glaciers and ice
- ocean currents and waves
- gravity
Chemical weathering
Dissolution or transformation of original minerals to secondary minerals by interaction with various solutions
- dissolution by water
- dissolution by acid
- oxidation
- hydrolysis (diagenesis)
Properties of clay
Good properties: -filtering of toxic metals -material for pottery and construction Bad properties: -swelling of soils -soil failures (slumps, landslide)
Factors that control the extent of chemical weathering
1) composition of minerals
2) temperature
3) presence of water (humidity)
Weathering-composition of minerals
- ferromagnesian silicates weather the fastest
- K - Al silicate are more resistant to weathering
- Halides and Sulfates dissolve easily in solutions
- carbonates dissolve easily in acidic solutions
Weathering-temperature
High temp increases rate of weathering
Role of climate
Climate combined the previously noted factors
- in warm, humid climates, chemical weathering predominates
- in arid, cold climates, mechanical weather predominates
Transporting sediment
- water (fluvial transport)
- glaciers
- wind (Aeolian transport)
- gravity (Mass wasting)