MATERIALS OF THE LITHOSPHERE
ROCKS
IGNEOUS
- most rocks in the earths crust are igneous in origin
- Formation of Igneous Rocks
- from the solidification of magmas
- temperature, pressure, and water are catalysts of rock melting
- partial melting
- since melted rock (liquid) has a lower density than solid rock, it rises in the earths crust where it accumulates in magma chambers
- Classification based on texture and composition
- Texture: size of individual grains / minerals
- phaneritic vs. aphanitic
- glassy
- porphyritic
- fast cooling = "fine" texture or "glassy"
- slow cooling = "course" texture
- Intrusive Igneous Rock Bodies
- magmas from the melting of mantle crustal rocks
- magmas rise, intrude into the crust
- Extrusive Igneous Rocks
- Lavas - pahoehoe, aa (viscosity)
- Pyroclastics (fire fragments)
- volcanic ash and tuff
- Volcanic Glass (pumice, scoria, obsidian)
- Porphyritic Igneous Rocks
- Volcanism: the process by which magma from the interior of the earth rises through the crust, emerges onto the surface as lava, and cools into volcanic rock
- Anatomy of a volcano (overhead)
- Types of lava (based on silica content)
- Types of Volcanic Deposits
- Basaltic: Flood Basalts, Pahoehoe, Aa, Pillow lava
- Rhyolitic
- Andesitic
- Textures: glassy, vesicular
- explosive vs. gentle eruptions
- Pyroclastic Deposits
- Air fall or tephra
- Ejecta: ash, tuffs and breccias, bombs
- Surge:
- nuée ardante (glowing cloud)
- Mudflow
- Landforms and Eruptive Styles
- Shield Volcanoes
- gentle eruptions consisting of basaltic lavas
- low silica and low viscosity
- fissure eruptions and flood basalts
- example: Mauna Loa
- Volcanic Domes
- explosive eruptions consisting of felsic volcanism
- high silica and high viscosity
- ash flows
- example: Mount St. Helens (1980)
- Cinder-Cones Volcanoes
- Composite Volcanoes (stratovolcano)
- alternating lava and pyroclastic eruptions
- Craters
- central depression at the summit of most volcanos
- Calderas (collapsed craters)
SEDIMENTARY
Sedimentary rocks cover 75% of the surface of the earth
- Types of Sedimentary Rocks
- Clastic (detrital)- fragments of other rocks
- Non-clastic - chemical precipitates and evaporites
- Formation of Sedimentary Rocks
- Weathering
- Transportation and Sorting
- abrasion
- rounding and sorting
- Deposition
- depositional environments
- Lithification
METAMORPHIC ROCKS
Metamorphism
process by which rocks undergo changes in mineralogy, texture, or chemical composition
- WHERE? in the crust and mantle
- Metamorphic Agents: internal heat, weight of rock, horizontal pressures of deformation result in:
- Types of Metamorphism
- Contact
- plate convergence
- oceanic and continental hot spots
- deformed mountain belts
- Regional
- plate subduction
- plate convergence
- Burial
ROCK CYCLE