Earth History Flashcards
Continental crust
Composed of variety of rock types
Much thicker
Lower density (2.7g/cm^3)
Silica-rich rocks such as granite
Supercontinents
Large landmasses that contain all or nearly all of the existing continents
Pangaea most recent
Rodinia
Earliest well documented supercontinent formed during Proterozoic eon
Gondwana
By end of Precambrian many fragments of rodinia reassembled to produce large landmass located in Southern Hemisphere. Sometimes considered a supercontinent.
Formation of Pangaea
During Paleozoic era
Collisions of N.America, Europe, Siberia + other smaller crystal fragments forming s larger northern continent called Laurasia
Gondwana migrated northward and collided with Laurasia to form Pangaea
Stromatolites
Limestone mats built by lime accretions bacteria
Cambrian explosion
Huge expansion in biodiversity during beginning of Paleozoic era, Cambrian period
Oceanic crust
Dense (3.0g/cm^3)
Homogenous layer of basaltic rocks derived from partial melting of the rocky, upper mantle
Thin
Cratons
Thin crustal fragments collide and accrete to form larger crustal provinces which assemble into larger blocks called cratons. Core of modern continent and mostly formed during Precambrian