Lab exam 1 Flashcards
Element->
minerals-rocks
Mineral
Naturally occurring, inorganic substance with fixed chemical compositions, a definite atomic structure, and characteristic set of physical properties.
Physical Properties
Luster Hardness Cleavage and Fracture Crystal form Color Conchodial Fracture- curved fracture Effervescence- fizzes with hydrochloric acid Greasy texture-soapy Salty Streak Striations- grooves or lines Specific Gravity- dense
Luster
Metallic and Non metallic
Metallic
reflects light like a metal pyrite
Nonmetallic
oVitreous/glassy- shiny like glass quartz
oDull- earth appearance hematite
Silky- fibrous gypsum
Pearly- reflect like a pearl
Hardness
- Finger nail 2.5, Penny 3.5, glass 5.5, Steel File 6
* Moh’s Scale of Hardness
Cleavage and Fracture
- N/A, 1 plane, 2 planes (60,90, 120)
- Not necessarily a flat surface
- Sharper corner cleavage
- Jagged corner fracture
- Focus on the edges
Crystal form
•Quartz
Rock
one or more minerals, aggregate of minerals
3 classifications
igneous, metamorphic, and sedimentary
Melting- magma
- decrease in pressure (pop in a bottle), adding water (subduction zones), hot spots
Solidification-
below the ground (intrusive) and above the ground (extrusive
Pyroclastic-explosive
- Scoria-dark, dense, red
- Pumice- floats and light in color
- Bombs- round and dark
- Tuff- ash
- Obsidian- black, glassy, conchoidal
Texture
- Phaneritic- grains are large enough to be seen (intrusive)
- Porphyritic- large grains two different sizes (intrusive then extrusive)
- Aphanitic- fine (extrusive)
Color
- Mafic- Dark, iron rich
- Intermediate- salt and pepper
- Felsic- light silica
Sedimentary Rocks
Rocks consist of material (sediment) from other locations. Most are sediment pieces or clasts, formed from weathering and erosion of other rocks. Material is accumulated at a new site, buried and lithified.
Weathering
physical or chemical processes that break down rocks
Erosion
transported by rivers, glaciers, waves, wind, and gravity alone
Lifthificaition
once sediment is deposited it is lithified through the processes of compaction and cementation.
Classification of clastic sedimentary
- Size- boulders, cobbles, pebbles, sand silt, and clay
- Sorting- poorly sorted, moderately sorted, and well-sorted
- Shape-angular and rounded
Non-clastic- extracted from water or organisms
Evaporites- rock salt
•Carbonate- limestone
•Siliceous- chert/flint
•Carbonaceous- coal
Walter’s law
telling enviroment form rock
Metamorphic Rock
Change in form, pre-existing sedimentary, igneous, or metamorphic rock. Cause the alignment of minerals, recrystallization of minerals, and growth of new minerals with the addition of heat, pressure, and or chemically active fluids. (Ex. Shale (low)-> Slate (high) -> gniess)
Heat-
increase the rate of chemical reaction in a rock, which can create changes in the mineral. Magma affects surrounding rock or subduction occurs
2 ways
intrusive magma or extrusive lava or earth naturally increase with depth (buried)
Pressure
rock is deep within the ground. Lithostatic pressure one direction. Differential pressure different direction
Chemically active fluid
water trapped between grains, fluids in magma, and water in water bearing minerals
Foliation
result of differential pressure, directs the rock in one direction (non-foliated. High to low foliation