
Continental drift
... • The liquid outer core surrounds the inner core and is believed to be composed of iron mixed with nickel and trace amounts of lighter elements • Recent studies suggests that the innermost part of the core is enriched in gold and platinum while also containing nickel and primarily iron • Extreme hea ...
... • The liquid outer core surrounds the inner core and is believed to be composed of iron mixed with nickel and trace amounts of lighter elements • Recent studies suggests that the innermost part of the core is enriched in gold and platinum while also containing nickel and primarily iron • Extreme hea ...
Document
... • Please IGNORE these….. • They are based on outdated information and will be marked wrong in geology exams • They often also show continental crust floating on oceanic crust, this is also incorrect. ...
... • Please IGNORE these….. • They are based on outdated information and will be marked wrong in geology exams • They often also show continental crust floating on oceanic crust, this is also incorrect. ...
The Ocean Floor Bethany Ostlund 4th Grade The Ocean Floor
... In the following diagram there is evidence of seafloor spreading by showing the ages of the ocean floor. The red colors are the youngest parts of the seafloor, where fresh new crust is formed as lava seeps up from the deep interior of the Earth at spreading ridges. The green colors are the spreading ...
... In the following diagram there is evidence of seafloor spreading by showing the ages of the ocean floor. The red colors are the youngest parts of the seafloor, where fresh new crust is formed as lava seeps up from the deep interior of the Earth at spreading ridges. The green colors are the spreading ...
LECTURE W14-15-L29-30
... created by cosmic rays + oxygen and nitrogen in upper atmos. Earth by precipitation & readily clay-rich oceanic seds ...
... created by cosmic rays + oxygen and nitrogen in upper atmos. Earth by precipitation & readily clay-rich oceanic seds ...
Accommodating sill-complex emplacement
... forced folds, sub-horizontal sills may evolve into laccoliths or obtain a saucer-shaped morphology. These analyses highlight that the behaviour of the host rock during emplacement strongly influences forced fold evolution and may also determine whether additional space-making mechanisms occur (e.g., ...
... forced folds, sub-horizontal sills may evolve into laccoliths or obtain a saucer-shaped morphology. These analyses highlight that the behaviour of the host rock during emplacement strongly influences forced fold evolution and may also determine whether additional space-making mechanisms occur (e.g., ...
Earthquakes
... – Scientists noticed that at about 2900 km at the mantle-core interface that P waves greatly slowed and S waves stopped, then the P waves increase again after 5200 km – Since S waves can’t pass through liquids and P waves move more slowly in liquids, this led to the conclusion that the outer core wa ...
... – Scientists noticed that at about 2900 km at the mantle-core interface that P waves greatly slowed and S waves stopped, then the P waves increase again after 5200 km – Since S waves can’t pass through liquids and P waves move more slowly in liquids, this led to the conclusion that the outer core wa ...
NORWOOD SCIENCE CENTER
... scientists tools to study these events in detail. The theory of plate tectonics has provided scientists with the ability to explain why they occur. ...
... scientists tools to study these events in detail. The theory of plate tectonics has provided scientists with the ability to explain why they occur. ...
Plate Tectonics Theory
... • It is not understood how this happens and what affect it might have on living organisms. • It does appear to be very strong evidence that the bottom of the ocean has spread. ...
... • It is not understood how this happens and what affect it might have on living organisms. • It does appear to be very strong evidence that the bottom of the ocean has spread. ...
Layering in the wall rock of Valles Marineris: intrusive and extrusive
... within terrestrial cumulate rocks can vary from tens of meters to centimeters. Though the origin of layering in intrusions is poorly understood, it is generally interpreted to result from fractional crystallization and sedimentary processes during crystallization in cooling magma chambers. Examples ...
... within terrestrial cumulate rocks can vary from tens of meters to centimeters. Though the origin of layering in intrusions is poorly understood, it is generally interpreted to result from fractional crystallization and sedimentary processes during crystallization in cooling magma chambers. Examples ...
8th Grade Science
... Identify the effects of convection currents on tectonic plates of Earth’s crust and upper mantle (volcanoes, earthquakes, ocean floor spreading, mountain building, faulting, and folding) Describe natural disasters, predict their effects, and classify them as constructive or destructive forces (earth ...
... Identify the effects of convection currents on tectonic plates of Earth’s crust and upper mantle (volcanoes, earthquakes, ocean floor spreading, mountain building, faulting, and folding) Describe natural disasters, predict their effects, and classify them as constructive or destructive forces (earth ...
Continental Drift - Ashland Independent Schools
... B. The ocean has high and low tides. C. One portion of the Earth’s crust dives beneath another portion. D. The oldest part of the ocean floor is found farthest from the mid-ocean ridge. ...
... B. The ocean has high and low tides. C. One portion of the Earth’s crust dives beneath another portion. D. The oldest part of the ocean floor is found farthest from the mid-ocean ridge. ...
Electrochemistry Lecture
... 2 Ca (s) + O2 2CaO Which is undergoing oxidation ? Reduction? Oxidation: Ca Ca+2 Reduction: O2 O-2 Oxidizing agent; That which is responsible to oxidize another. O2 ; Oxidizing agent; The agent itself undergoes reduction ...
... 2 Ca (s) + O2 2CaO Which is undergoing oxidation ? Reduction? Oxidation: Ca Ca+2 Reduction: O2 O-2 Oxidizing agent; That which is responsible to oxidize another. O2 ; Oxidizing agent; The agent itself undergoes reduction ...
plate tectonics - Math/Science Nucleus
... rigid, they tend to stick together, even though they are constantly moving. When the strength of the rocks at the plate boundary is exceeded, they move rapidly, “catching up” with the rest of the plates. We feel this release of energy as an earthquake. Many lines of evidence indicate that the plate ...
... rigid, they tend to stick together, even though they are constantly moving. When the strength of the rocks at the plate boundary is exceeded, they move rapidly, “catching up” with the rest of the plates. We feel this release of energy as an earthquake. Many lines of evidence indicate that the plate ...
2 Regional Geological Setting
... Due to the on-going controversial discussion about the stratigraphical positions of the different lithotypes, this metallogenic study uses lithological terms rather than stratigraphical terms. The stratigraphical terms are also avoided, since this study is based mainly on drill core data that did no ...
... Due to the on-going controversial discussion about the stratigraphical positions of the different lithotypes, this metallogenic study uses lithological terms rather than stratigraphical terms. The stratigraphical terms are also avoided, since this study is based mainly on drill core data that did no ...
platetectonics
... two layers: a solid inner core and a liquid outer core. The middle layer of the Earth, the mantle, is made of minerals rich in the elements iron, magnesium, silicon, and oxygen. The crust is rich in the elements oxygen and silicon with lesser amounts of aluminum, iron, magnesium, calcium, potassium, ...
... two layers: a solid inner core and a liquid outer core. The middle layer of the Earth, the mantle, is made of minerals rich in the elements iron, magnesium, silicon, and oxygen. The crust is rich in the elements oxygen and silicon with lesser amounts of aluminum, iron, magnesium, calcium, potassium, ...
PPT Oxidation
... reduced and get oxidized. Here are the two halfreactions from the example: Ag+ ---> Ag Cu ---> Cu2+ • The silver is being reduced, its oxidation number going from +1 to zero. The copper's oxidation number went from zero to +2, so it was oxidized in the reaction. In order to figure out the halfreacti ...
... reduced and get oxidized. Here are the two halfreactions from the example: Ag+ ---> Ag Cu ---> Cu2+ • The silver is being reduced, its oxidation number going from +1 to zero. The copper's oxidation number went from zero to +2, so it was oxidized in the reaction. In order to figure out the halfreacti ...