california rock stories linking tectonics to rock formation ellen metzger baesi – october 8, 2011
TRANSCRIPT
California’s Rocks
• California, including the Bay Area, has a greater variety of rocks than do other regions of the United States.
• This reflects the state’s complex tectonic/geologic history.
Mineral Hazards
• Serpentinite California state rock Metamorphosed ultramafic rocks from the
mantle (can you find these rocks on your California geologic map?)
There are several minerals in the serpentine groupChrysotile is asbestiform
Mineral Hazards: Mercury in the Environment
• Mercury is a neurotoxin – principal source for humans: consumption of mercury-contaminated fish
• Sources of mercury in the environmentNatural sources:
Volcanoes, hot springs, and natural mercury deposits (the mineral cinnabar (HgS)is an ore of mercury
Sources related to human activities: coal combustion, incineration of waste, industrial activities, mining
Source: California Geological Survey
Source: BLM
Bay Area Rocks
• Young sedimentary and volcanic rocks
• Mesozoic rocks Franciscan Complex Coast Range Ophiolite Great Valley Group
• Salinian basement
Cross section of western North America at about 100 million years ago/www.nps.gov/prsf/naturescience/images/Subduction-animation_1.gif
California tectonics in the past: a subduction zone
Unique Bay Area Rocks
• Igneous Sea floor basalt
Pillow lavasGreenstone (altered basalt)
• Sedimentary Graywacke (“dirty” sandstone) Radiolarian Chert
Radiolarians: Tiny ocean animals that make their skeletons of silica (SiO2) http://www.mdia.org/images/Radiolaria.jpg
Unique Bay Area Rocks
• MetamorphicGlaucophane schist (“blueschist”) formed
under high P-low T in a subduction zone.Serpentinite - hydrated mantle rocks
Mantle rock = ultramafic (Si02-poor), dense, dark Serpentinite = rock (CA State Rock) Serpentine = mineral Should serpentinite be “demoted” as our state
rock?