geology of the feather river
DESCRIPTION
Geology of the Feather River. Where does one start? NERDS 2006 Teresa Kennedy. Some Understandings. Plate Tectonics (which is different from continental drift) Subduction results in remelted material (magma) which rises because it is less dense to form new crust - PowerPoint PPT PresentationTRANSCRIPT
Geology of the Feather Geology of the Feather RiverRiver
Where does one start?Where does one start?
NERDS 2006NERDS 2006
Teresa KennedyTeresa Kennedy
Some UnderstandingsSome Understandings
Plate Tectonics (which is different from Plate Tectonics (which is different from continental drift)continental drift)
Subduction results in remelted material Subduction results in remelted material (magma) which rises because it is less (magma) which rises because it is less dense to form new crustdense to form new crust
Plate margins are places of brittle and Plate margins are places of brittle and ductile deformationductile deformation
The past is the key to the present…The past is the key to the present…geologic processes are dynamicgeologic processes are dynamic
Geologic Time ScaleGeologic Time Scale
Four Major Eras:Four Major Eras: Precambrian: Age of AlgaePrecambrian: Age of Algae Paleozoic: Age of FishPaleozoic: Age of Fish Mesozoic: Age of DinosaursMesozoic: Age of Dinosaurs Cenozoic: Age of MammalsCenozoic: Age of Mammals
OverviewOverview
Igneous, metamorphic, and sedimentary Igneous, metamorphic, and sedimentary rocksrocks
Some tilted, some flat-lyingSome tilted, some flat-lying Submarine and subaerial rocksSubmarine and subaerial rocks Much of the rock record missing due to Much of the rock record missing due to
erosionerosion FossilsFossils Heavy vegetationHeavy vegetation GlaciationsGlaciations
PrecambrianPrecambrian
~ 4.5 billion years ago~ 4.5 billion years ago Until 544 million years ago…Until 544 million years ago… Feather River area was at the bottom Feather River area was at the bottom
of the oceanof the ocean No rocks this old are exposed No rocks this old are exposed
anywhere close to there!anywhere close to there!
PaleozoicPaleozoic
544 million years to 255 million years ago544 million years to 255 million years ago Western margin of North American craton Western margin of North American craton
was 600 – 700 miles to the eastwas 600 – 700 miles to the east 20,000 – 30,000 feet of rock deposited in 20,000 – 30,000 feet of rock deposited in
deep oceandeep ocean Chert (formed from radiolaria)Chert (formed from radiolaria) Volcanic ash and breccia from volcanoes Volcanic ash and breccia from volcanoes
caused by subduction to west.caused by subduction to west.
MesozoicMesozoic
225 million years to 65 million years225 million years to 65 million years Deformation: folding and faulting Deformation: folding and faulting
from collision with other crustal from collision with other crustal piecespieces
Layers tilted up to 60 degreesLayers tilted up to 60 degrees Metamorphism from igneous plutons Metamorphism from igneous plutons
rising from subducted magma.rising from subducted magma. Oldest plutons are to the westOldest plutons are to the west
CenozoicCenozoic
65 million years to present65 million years to present Modern volcanic activity related to Modern volcanic activity related to
spreading of Basin and Rangespreading of Basin and Range Crest of Sierra Nevada is to the westCrest of Sierra Nevada is to the west UpliftUplift
• ErosionErosion• Change in climateChange in climate
GlaciersGlaciers• ErosionErosion• Changes in drainage, soils, vegetationChanges in drainage, soils, vegetation