
Plates of the Lithosphere - Cal State LA
... Evidence of Continental Drift • Fossils – Animal and plant fossils appeared to have evolved in the same geographic region but now scattered on separate continents ...
... Evidence of Continental Drift • Fossils – Animal and plant fossils appeared to have evolved in the same geographic region but now scattered on separate continents ...
A1980JF47100001
... summer of 1963 for more detailed experiments. Maurice felt very strongly that though geophysical experiments were elegant and informative, it was important to find out something about the rocks on which the measurements were being made. This was an unfashionable view at the time, but I had been draf ...
... summer of 1963 for more detailed experiments. Maurice felt very strongly that though geophysical experiments were elegant and informative, it was important to find out something about the rocks on which the measurements were being made. This was an unfashionable view at the time, but I had been draf ...
Terms and Definitions 2017 File
... Where liquid rock rises up through a crack in the crust. Igneous rock Rock formed from cooled molten rock eg basalt. Sedimentary rock Rock formed from grains of eroded rock, plant and animal material, that has been pressed together eg limestone. Metamorphic rock Rock formed when sedimentary rock is ...
... Where liquid rock rises up through a crack in the crust. Igneous rock Rock formed from cooled molten rock eg basalt. Sedimentary rock Rock formed from grains of eroded rock, plant and animal material, that has been pressed together eg limestone. Metamorphic rock Rock formed when sedimentary rock is ...
EQ AND INTERIOR
... The map shows recent earthquake activity (red circles occurred today, etc.) so you can see just how common earthquakes are (over 1 million per year that can be recorded on seismometers!). Below the IRIS earthquake map, click on “Last 30 days earthquakes” which will give you a list of the most recent ...
... The map shows recent earthquake activity (red circles occurred today, etc.) so you can see just how common earthquakes are (over 1 million per year that can be recorded on seismometers!). Below the IRIS earthquake map, click on “Last 30 days earthquakes” which will give you a list of the most recent ...
Plate tectonics/boundaries
... Oceanic- continental: More dense oceanic crust is subducted under the continental crust, melts, & rises causing volcanic mountains to form on the continent. Oceanic- oceanic: The more dense plate is subducted, melts, & rises causing a volcanic island arc. Continental- continental: Neither plate gets ...
... Oceanic- continental: More dense oceanic crust is subducted under the continental crust, melts, & rises causing volcanic mountains to form on the continent. Oceanic- oceanic: The more dense plate is subducted, melts, & rises causing a volcanic island arc. Continental- continental: Neither plate gets ...
Chapter 3 - Igneous Rocks
... Correlation: Using relative dating techniques to date a sequence of sedimentary strata and structures. Relative dating problem, e.g. #21 from Ch. 18 Absolute Dating with Radioactivity Radioactivity – an unstable element decays, by gaining or losing nuclear particles, and becomes another, more ...
... Correlation: Using relative dating techniques to date a sequence of sedimentary strata and structures. Relative dating problem, e.g. #21 from Ch. 18 Absolute Dating with Radioactivity Radioactivity – an unstable element decays, by gaining or losing nuclear particles, and becomes another, more ...
Plate_tectonics[1]
... were not accepted at first • Wegener believed the landmass broke apart 200 million years ago • Continental drift is the idea proposed by Wegener that the continents have drifted horizontally to their current locations, ...
... were not accepted at first • Wegener believed the landmass broke apart 200 million years ago • Continental drift is the idea proposed by Wegener that the continents have drifted horizontally to their current locations, ...
Geologic Dating
... –Rocks of the crust provide clues to Earth’s past • By analyzing these clues we can infer events from the past ...
... –Rocks of the crust provide clues to Earth’s past • By analyzing these clues we can infer events from the past ...
Earth 50: Plate Tectonics 9-25-06 Continental Drift James Hutton
... James Hutton—concept of a “World Machine” that renews itself. Erosion tears at mountains, creating sediments that pile up in the ocean, eventually melt, and are uplifted becoming new mountains. A cycle with no end; a static world of vertical movements but no moving continents Alfred Wegner: Recogniz ...
... James Hutton—concept of a “World Machine” that renews itself. Erosion tears at mountains, creating sediments that pile up in the ocean, eventually melt, and are uplifted becoming new mountains. A cycle with no end; a static world of vertical movements but no moving continents Alfred Wegner: Recogniz ...
a 22 page PDF of this title
... In some places, the continents look as if they would fit together like jigsaw-puzzle pieces if the intervening ocean were removed. In 1620, Francis Bacon also wrote of a “certain correspondence” between shorelines on either side of the South Atlantic. Figure 3.1 shows this remarkable appearance. Cou ...
... In some places, the continents look as if they would fit together like jigsaw-puzzle pieces if the intervening ocean were removed. In 1620, Francis Bacon also wrote of a “certain correspondence” between shorelines on either side of the South Atlantic. Figure 3.1 shows this remarkable appearance. Cou ...
CHAPTER 3CPLATE TECTONICS
... the earth was considered to be too young for the continents to have moved any appreciable distance. d. the positions of the continents on ancient maps were the same as on modern maps. 3. The lithosphere a. is partly molten and plastic in consistency. b. was discovered by studying the behavior of sei ...
... the earth was considered to be too young for the continents to have moved any appreciable distance. d. the positions of the continents on ancient maps were the same as on modern maps. 3. The lithosphere a. is partly molten and plastic in consistency. b. was discovered by studying the behavior of sei ...
answers to review questions – chapter 33
... Pre-Cambrian—origins of life Palaeozoic—ancient life Mesozoic—age of dinosaurs Cenozoic—the beginning of modern life Older Pre-Cambrian organisms were prokaryotes. Some of these prokaryotes were photosynthetic which, in addition to the evolution of first life during this era, is the most significant ...
... Pre-Cambrian—origins of life Palaeozoic—ancient life Mesozoic—age of dinosaurs Cenozoic—the beginning of modern life Older Pre-Cambrian organisms were prokaryotes. Some of these prokaryotes were photosynthetic which, in addition to the evolution of first life during this era, is the most significant ...
They believe that 200 million years ago, some force made Pangaea
... People need fresh water—the Earth has enough, but some places have too much, and others have too little. ...
... People need fresh water—the Earth has enough, but some places have too much, and others have too little. ...
Life and the Evolution of Earth`s Atmosphere
... atmosphere was probably several times denser than what we have now, and was dominated not by oxygen, but by carbon dioxide—a major greenhouse gas. Other gases, such as molecular nitrogen, water vapor, and small amounts of carbon monoxide, sulfur gases, and trace quantities of methane, and hydrogen w ...
... atmosphere was probably several times denser than what we have now, and was dominated not by oxygen, but by carbon dioxide—a major greenhouse gas. Other gases, such as molecular nitrogen, water vapor, and small amounts of carbon monoxide, sulfur gases, and trace quantities of methane, and hydrogen w ...
Revision Booklet
... What and where? On 26 December 2004 a tsunami occurred in the Indian Ocean. It was the result of the Indio-Australian Plate sub-ducting below the Eurasian Plate. It was caused by an earthquake measuring more than magnitude 9. The earthquake caused the seafloor to uplift, displacing the seawater abov ...
... What and where? On 26 December 2004 a tsunami occurred in the Indian Ocean. It was the result of the Indio-Australian Plate sub-ducting below the Eurasian Plate. It was caused by an earthquake measuring more than magnitude 9. The earthquake caused the seafloor to uplift, displacing the seawater abov ...
Worksheets - Keep It Simple Science
... a) The crust keeps splitting open in the middle and new crust rock forms in the gap. This is why the rock is youngest in the middle and gets older outwards. This also explains the symmetrical pattern of magnetism on either side of middle. b) Furthest away from the centre, because the oldest rocks ha ...
... a) The crust keeps splitting open in the middle and new crust rock forms in the gap. This is why the rock is youngest in the middle and gets older outwards. This also explains the symmetrical pattern of magnetism on either side of middle. b) Furthest away from the centre, because the oldest rocks ha ...
View Sample
... Rocks of the oceanic crust are often referred to as sima this refers to their most common mineral components silica and magnesium Layer 2- The mantle This is the layer directly below the crust. It has the following features: It is nearly 3000 km thick we can divide it into the upper, middle and lowe ...
... Rocks of the oceanic crust are often referred to as sima this refers to their most common mineral components silica and magnesium Layer 2- The mantle This is the layer directly below the crust. It has the following features: It is nearly 3000 km thick we can divide it into the upper, middle and lowe ...
UNIT PLAN 2A: PLATE TECTONICS
... force. C. Wegener could not explain how or why the continents moved.* D. Wegener thought that the south pole had changed position. 10.Which of the following was NOT used by Wegener to support his hypothesis that the continents had once been joined as one. A. fossils of land-dwelling animals ...
... force. C. Wegener could not explain how or why the continents moved.* D. Wegener thought that the south pole had changed position. 10.Which of the following was NOT used by Wegener to support his hypothesis that the continents had once been joined as one. A. fossils of land-dwelling animals ...
Juniata College Shake, Rattle, and Roll Earthquake Board and
... and observes that an object on the other side moves to the right during an earthquake, the fault is called a right-lateral strike-slip fault (like California's San Andreas fault). If the object moves to the left, the fault is called a left-lateral strike-slip fault. Subduction zone boundary -The reg ...
... and observes that an object on the other side moves to the right during an earthquake, the fault is called a right-lateral strike-slip fault (like California's San Andreas fault). If the object moves to the left, the fault is called a left-lateral strike-slip fault. Subduction zone boundary -The reg ...
10 - Aurora City Schools
... Tectonic plates are huge rigid plates that move extremely slowly atop the denser mantle. They were likely formed from the flows of energy and heated material in convection cells that caused the lithosphere to break up. Tectonic plates can also slide and grind past one another along a fracture (fault ...
... Tectonic plates are huge rigid plates that move extremely slowly atop the denser mantle. They were likely formed from the flows of energy and heated material in convection cells that caused the lithosphere to break up. Tectonic plates can also slide and grind past one another along a fracture (fault ...
Geophysics

Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.