CEE 437 Lecture 4 Igneous and Metamorphic Rocks, Rock Lab October 10, 2002 Thomas Doe
Outline Igneous Rocks Metamorphic Rocks Rock Identification Lab
Northwest Igneous and Metamorphic Rocks Columbia River Basalts (miocene) Snake River Basalts (pliocene ) Yellowstone Region Acidic Volcanics (Pleistocene to recent) Cascade Volcanoes (recent) Recent Basaltic Volcanism (Newberry Crater) Cascade Batholiths (Felsic, Cret- Miocene)
Geologic Settings for Igneous Rocks Oceanic –Hi Fe, Mg, Ca, low Si –basalt, gabbro Continental –Hi Si, Na, K –granite, rhyolite, andesite
Igneous Origins Intrusive –Batholithic or plutonic: phaneritic –Dikes or sills that chill rapidly: aphanitic Extrusive –deposition as melt (lava) –pyroclastic tuff tephra pyroclastic flows
Identifying Igneous Rocks Chemistry –Acidic: Basic (more Si, less Si) Texture –Aphanitic: crystals not visible –Phaneritic: made of visible crystal components –Porphyritic: Larger crustals in aphanitic or phaneritic ground mass
Igneous Rock Identification
Igneous Rock Classification SERPENTINITE Acidic, FelsicBasic, MaficUltramafic Common Types in RED outline
Igneous Structural Features
Magma Generation on Continental Margins
Magma Generation in Convergent Continental Plate Margins
Igneous Structures
Extrusives Viscosity varies with Si and water content –Basalt — low viscosity –Rhyolite — high viscosity Rhyolite flows relatively unusual as rhyolite does not flow well –Explosive –Tuffs, pyroclastics
Volcano Types Basaltic: low viscosity — Hawaii, Columbia Plateau Andesitic/Rhyolitic
Structures of Basalt Flows Lava Tubes Flow Stratigraphy –collonade –entablature –flow top breccia/scoria
Hawaii Basalt Flows
Basalt Flow Structures
Eruptions of Acid-Rock Volcanoes
Rhyolite Dome
Caldera
Mt. St. Helen’s Blast Zone
Mt. Mazama Ash Distribution
Subduction-Zone Metamorphism
Metamorphism Recrystallization of Rock Under Temperature and Pressure
Metamorphic Rock Classification
Metamorphic Classification Original Material –sandstone, limestone, shale, basalt) Metamorphic Grade (Temperature, Pressure) Source of Metamorphism (Regional, Contact)
Basic Metamorphic Types Quartz Sandstone Quartzite Limestone, Dolomite Marble Shale –Slate — cleavage, no visible xl’s –Phyllite — foliation, mica sheen but xl’s not visible –Schist — clear foliation, visible mica –Gneiss — like granite but with foliation/gneissosity Basalt greenschist, amphibolite
Origin of Foliation (gneissosity, schistosity)
Metamorphism at Continental Collisions
Contact Metamorphism
Metmorphic Grade
Northwest Igneous and Metamorphic Rocks Columbia River Basalts (miocene) Snake River Basalts (pliocene ) Yellowstone Region Acidic Volcanics (Pleistocene to recent) Cascade Volcanoes (recent) Recent Basaltic Volcanism (Newberry Crater) Cascade Batholiths (Felsic, Cret- Miocene)
Sauk River Quadrangle
Malpasset Dam