Geology is the study of planet Earth and its history, also known as Earth Science or Geoscience
Physics is the study of elemental matter and energy
Geophysics is the application of physics to geology
The hard rocky surface is called lithospheric plates and moves 25 cm/yr
Tectonics means "to build" and includes plate tectonics (continents sliding above hot plastic rocks) and vertical tectonics (mantle plumes of hot rock outpouring magma)
Divergent plate margin involves continuous addition of new magma and its cooling, resulting in continuous movement of the plate away from the spreading center
Orogeny refers to plates colliding and joining, creating convergent plate margins
Subduction occurs when plates collide and one is destroyed
Pangea was a supercontinent
Uniformitarianism is the reconstruction of ancient environments by studying rock records, with the principle that "the present is the key to the past"
Hydrogeology is the study of underground water, while hydrology is the study of surface water
Sir Francis Bacon first suggested that all continents were together
Antonio Snider-Pellegrini drew pictures demonstrating continents fitting together
The first atlas of the Earth was made by Abraham Ortelius in 1598
In 1683, the first European saw Niagara George and estimated the age of the Earth
James Hutton, the "father of geology," published the theory of the Earth in 1795
Charles Lyell's uniformitarianism states that the same natural laws and processes have always operated
Robert Mallet coined the terms seismic and epicenter
In 1846, Robert Mallet proposed that earthquakes are generated by crystal movements
Antonio Snider noticed similarities in fossil assemblages of plants in Europe and America in 1858
Lord Kelvin estimated the age of the Earth to be 100 million in 1862
In 1872, the mid-Atlantic ridge and Challenger deep were discovered
Ernest Rutherford's nuclear decay theory in 1905 predicted the Earth's age
Jean Brühnes indicated that the North Pole was once at the South Pole in 1906
Hess and Dietz proposed sea floor spreading in 1961
Arthur Holmes proposed that continental drift is explained by convection currents in the mantle
Tuzo Wilson invented the Wilson cycle, which explains the growth and decay of supercontinents
Carl Schuchert's permanentism and Frank Bursley Taylor's mobilism theories
Alfred Wegener coined the term Pangea and wrote "The Origin of Continents and Oceans"
The discovery of magnetic stripes on the ocean floor supported the theory of sea floor spreading
Harold Hess introduced sea floor spreading, leading to the abandonment of permanentism
Transform faults allow spreading on either side of mid-ocean ridges
Focus is where an earthquake is generated, while the epicenter is directly above on the Earth's crust
Seismographs detect seismic waves
Types of tectonic plates and plate margins: divergent, convergent, and transform
Divergent boundaries contribute to seafloor spreading, producing oceanic crust
Convergent boundaries involve plates moving toward each other, creating subduction or obduction zones
Transform boundaries are where plates slide sideways past each other