Test 1 Flashcards
Hardness
Resistance to abrasion, mobs scale of hardness
Cleavage
Tendency for mineral to split along a plane (along weak bonds of Chrystal lattice
Solubility
Use of dilute acid to identify carbonate minerals
Rock characteristics
Type, age, place, structure
Rock mass
Rock material + deformation/defects
Describe two rocks you would find at the younger end of the standard geologic column scale
Holocene, Pleistocene
Igneous rock
Solidified from molten material (magma), volcanic, plutonic
Sedimentary rock
Mechanically deposited, organically deposited, littified in place (turn to stone)
Occurrences of igneous rocks
Plutonic - high pressure environment, slow cooling, intrusive plutons. Sub volcanic - transitional between 1 and 3, intrusive sills and dykes. Volcanic - law pressure environment, fast cooling, extrusive.
Magma
Molten rock forming when temperatures rise and melting occurs in the mantle or crust. Less dense than surrounding rock so rises buoyantly. As magma cools Chrystals of different minerals form.
Aphanitic and phaneritic and porhyritic rock texture
Fine grained-rapid cooling (days to months). Coarse grained (slow cooling over centuries). Large Chrystals in fine grained matrix more than one stage of cooling (combination).
Plutonic rock
Formed at depth within crust, cools slowly (coarse grained), non-vesicular (no bubbles in rock mass), exposed at surface by uplift and erosion.
Volcanic rock effusive activity
Magma extruded at the ground surface, lava flows and lava domes, forms crystalline igneous rocks.
Volcanic rock explosive activity
Forms range of rock types, lava-fire fountahing, pyroclasts/tephra, ignimbrites - from pyroclastic flows, lahar
Types of lava
Basalt, andesite, rhyolite, nigh viscosity lava will how slowly and form semi rigid blocks, allows trapped gas and vesicles to form. Low viscosity flows easily, gas is released.