chapter 12
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anthropocene
age of human transformation of Earth’s biological and physical systems
how old is our solar system
4.6 billion
how was earths atmosphere formed?
gases emmitted by volcanos
what are cynobacteria?
photosynthetic bacteria that helped put oxygen into our atmopshere
stromatolites
colonies of cyanobacteria. fossils date back to 3.5 bill years
how old is earth
4.6 bill
uniformitarianism:
the principle that the same gradual and nearly imperceptible processes operating now have operated in the past
how do scientists date materials
relative age: compares age of one object or event with age of another without specifying how old either is — accounts for order of events Absolute age: an age that is specified in years before the present
superposition principle:
In a sequence of rock layers, the oldest rocks are at the bottom, and the youngest rocks are at the top
what 2 methods can determine absolute age
dendrochronology (tree ring analysis) Radiometric dating
what are the 3 principle layers of the earths interior
CoreMantleLithosphere
inner core:
composed of solid iron and nickelExtends from Earth’s center to about 5,150 km (3,200 mi) below Earth’s surfac
outer core:
composed of liquid iron and nickelExtends to about 2,900 km (1,800 mi) below Earth’s surface
what are the 2 types of crust
continental and oceanic
difference between magma and lava
Magma: melted rock that is below the surface of the crust. Often hardens into granite Lava: magma that spills onto the surface of Earth’s crustOften hardens into basalt