The Cooling Process, where cooling caused contraction and pressure that allowed some parts of the crust to rise and form mountains, while others buckled downward and formed ocean basins and other depressions
Isostasy Theory
Clarence Edward Dutton proposed the term "Isostasy" in 1889 to explain the concept of a contracting Earth, where equilibrium of the mass is applied
Continental Drift Theory
Alfred Wegener proposed it in his book "theOriginsofcontinentsandOcean" in 1915, it is the movement of Plate Tectonics
Tectonic
Derived from the Greek word "tekton" which means "carpenter" or "builder"
Tectonic Plates (also known as litospheric plates)
Massive slabs of solid rock that surround the earth's surface
Theatrum Orbis terrarum
The firstworldatlas, developed and published by Abraham Ortelius on January 1, 1596
Rodinia
A super continent that existed before Pangaea (meaning All Earth)
Pangaea
Began to split into 2 smaller supercontinents: Laurasia and Gondwanaland
Panthalassa
A vast ocean that surrounded Pangaea
Thetys
The sea that separated the 2 continents
Continental Plates
The solid ground on which you stand, made up of lower-density materials like granitic rock
Oceanic Plate
Heavier basalt and gabbro rocks that make up oceanic crust
Paleontological Evidence
Certain fossils on both sides of the Atlantic have a striking similarity that is difficult to explain if the continents were not once connected as one
Paleontological Evidence
Lystrosaurus & Cynognathus - 2 land dwelling reptiles that lived during the Triassic Period
Antonio Snider Pellegrini - used identical plant fossils
Edward Suess - described how plants in late paleozoic coal beds in india, Australia, south Africa and south America were all similar
Glossopteris - seed fern
Glaciation
An interval of time within the ice age that is marked by colder temperatures and glacier advances
Interglaciation / Interglacial
Warmer climates within an ice age
EvidencefromStructureandRocktype
Geographers noticed that the coastlines of several modern continents, would perfectly fit together
EvidencefromPaleoclimates
Wegener reconstructed and climatic zones using the distribution of specific rock types to determine the distribution of climates in ancient times to demonstrate the apparent shifting of climatic belts over time
Paleoclimatology
Study of the extended climatic conditions of past geologic conditions
Paleomagnetism
Study of ancient magnetic fields
Magnetometer
A sensitive instrument that scientists can determine the direction of the magnetic poles and the magnetic latitude