Class notes: Earth`s Interior
... They show several layers or zones inside Earth (Similar to X-rays) The deepest drill hole on Earth is only 12-16 km Less than 0.2 % of the distance to the core Layers of the Earth (See ESRT page 10) ...
... They show several layers or zones inside Earth (Similar to X-rays) The deepest drill hole on Earth is only 12-16 km Less than 0.2 % of the distance to the core Layers of the Earth (See ESRT page 10) ...
Word format - University of Idaho
... The father of modern geology, James Hutton, hypothesized that the Earth was much older than had previously been suggested. He promoted a concept called the Principle of Uniformitarianism, which essentially states: A. the present is the key to the past B. the past is the key to the future C. the past ...
... The father of modern geology, James Hutton, hypothesized that the Earth was much older than had previously been suggested. He promoted a concept called the Principle of Uniformitarianism, which essentially states: A. the present is the key to the past B. the past is the key to the future C. the past ...
plate tectonics
... Plate Tectonics- theory that Earth’s crust and upper mantle (lithoshphere) are broken into sections called plates that move on top of the asthenosphere. ...
... Plate Tectonics- theory that Earth’s crust and upper mantle (lithoshphere) are broken into sections called plates that move on top of the asthenosphere. ...
Earth and Space Science 2015 Semester 2 Exam Review Part 1 Convection
... along the fault can start an earthquake. Major fault lines can occur on or along plate boundaries. ...
... along the fault can start an earthquake. Major fault lines can occur on or along plate boundaries. ...
Description Crust Mantle Liquid Outer Core Solid
... separated into inner and outer core units. The inner core is a solid with a radius of about 1220km and the outer core, which does not permit the passage of shear waves, is liquid. ...
... separated into inner and outer core units. The inner core is a solid with a radius of about 1220km and the outer core, which does not permit the passage of shear waves, is liquid. ...
Royal Swedish Academy of Sciences
... extensional and compressional boundary zones between the plates are the scenes of the real action, with major earthquakes, volcanic eruptions, large displacements and mountain building. Plate motion is maintained by convection created by the Earth’s heat engine. McKenzie’s early numerical modelling ...
... extensional and compressional boundary zones between the plates are the scenes of the real action, with major earthquakes, volcanic eruptions, large displacements and mountain building. Plate motion is maintained by convection created by the Earth’s heat engine. McKenzie’s early numerical modelling ...
Coso Volcanic Field - Classes Dma Ucla Edu
... contribute to global warming, acid rain, and noxious smells if released. (source) ...
... contribute to global warming, acid rain, and noxious smells if released. (source) ...
Igneous Rocks Notes
... After the Earth formed, the planet’s interior became so hot that magma formed. Lava repeatedly flowed over the surface and hardened, forming a rocky crust. That crust sank into Earth’s interior, allowing more lava to erupt over the surface and harden to form rock. ...
... After the Earth formed, the planet’s interior became so hot that magma formed. Lava repeatedly flowed over the surface and hardened, forming a rocky crust. That crust sank into Earth’s interior, allowing more lava to erupt over the surface and harden to form rock. ...
Layers of The Earth - Songs for Teaching
... Go a lil’ deeper, 1600 Fahrenheit Let me put it in perspective Boiling water is a breeze I bet you ain’t know That’s only 2-1-2 degrees The crust consists of mainly two states First oceanic, second continental plates They float around On the second layer of the Earth All up on the mantle But that's ...
... Go a lil’ deeper, 1600 Fahrenheit Let me put it in perspective Boiling water is a breeze I bet you ain’t know That’s only 2-1-2 degrees The crust consists of mainly two states First oceanic, second continental plates They float around On the second layer of the Earth All up on the mantle But that's ...
Volcanic
... 1. Intrusive Igneous Forms Magma solidified at great depth (so mineral sizes are large) Plutons (individual magma chambers) Batholiths (merged magma chambers) ...
... 1. Intrusive Igneous Forms Magma solidified at great depth (so mineral sizes are large) Plutons (individual magma chambers) Batholiths (merged magma chambers) ...
Causes of Volcanic Eruptions
... Boundaries Most volcanic activity on Earth occurs at mid-ocean ridges. The next slide shows how magma forms at divergent boundaries such as those found along midocean ridges. ...
... Boundaries Most volcanic activity on Earth occurs at mid-ocean ridges. The next slide shows how magma forms at divergent boundaries such as those found along midocean ridges. ...
What type of boundary is…
... The lithosphere is Earth’s crust plus the rigid upper part of Earth’s mantle. The map shows plates of the lithosphere. What does the map tell you about the plates? A The plates are all moving in the same direction. B The plates are all the same size. C Plates and continents are different. ...
... The lithosphere is Earth’s crust plus the rigid upper part of Earth’s mantle. The map shows plates of the lithosphere. What does the map tell you about the plates? A The plates are all moving in the same direction. B The plates are all the same size. C Plates and continents are different. ...
topic 4 – the moving crust
... - A Canadian scientist that contributed to the theory of plate tectonics by suggesting that plates could also slide past each other. ...
... - A Canadian scientist that contributed to the theory of plate tectonics by suggesting that plates could also slide past each other. ...
Volcanoes and Plate Tectonics
... • Hot rock forced toward the crust where it melts partially to form a hot spot. • Pacific Plate is moving over a stationary hot spot. ...
... • Hot rock forced toward the crust where it melts partially to form a hot spot. • Pacific Plate is moving over a stationary hot spot. ...
millionaire 2nd version
... What is the type of rocked formed when heat and pressure change the rock into another rock entirely? A. Sedimentary ...
... What is the type of rocked formed when heat and pressure change the rock into another rock entirely? A. Sedimentary ...
Name____________________________
... Oceanic Crust: Dense crust formed by seafloor spreading at Mid-Ocean Ridges. Continental Crust: Less-dense crust that makes up the continents. Continental Drift: A theory stating that the Earth's continents have been joined together and have moved away from each other at different times in the Earth ...
... Oceanic Crust: Dense crust formed by seafloor spreading at Mid-Ocean Ridges. Continental Crust: Less-dense crust that makes up the continents. Continental Drift: A theory stating that the Earth's continents have been joined together and have moved away from each other at different times in the Earth ...
12.1 Notes - power point
... Ridge, a long mountain range running down the middle of the Atlantic Ocean. ...
... Ridge, a long mountain range running down the middle of the Atlantic Ocean. ...
Powerpoint presentation for Lecture 3 - e
... magnetic moment when they are cooled below the Curie Temperature ...
... magnetic moment when they are cooled below the Curie Temperature ...
HNRS 227 Lecture #17 & 18 Chapters 12 and 13
... pressure, or hot solutions into a distinctly different rock.” • See Figure 14.12 in textbook ...
... pressure, or hot solutions into a distinctly different rock.” • See Figure 14.12 in textbook ...
Structure of the earth
... • the outer layer of the earth is composed of soil and solid rock • Continental crust- composed primarily of granite, is thicker sedimentary and metamorphic rocks which form the continents • Oceanic crust- composed primarily of basalt, is thinner. ...
... • the outer layer of the earth is composed of soil and solid rock • Continental crust- composed primarily of granite, is thicker sedimentary and metamorphic rocks which form the continents • Oceanic crust- composed primarily of basalt, is thinner. ...
Name
... the stability of a slope can be caused by; an absence of vegetation, erosion of the toe of a slope by running water, or weakening of the slope by water saturation from snowmelt or heavy rains. The shaking of the ground by earthquakes or volcanic activity can often trigger landslides. ...
... the stability of a slope can be caused by; an absence of vegetation, erosion of the toe of a slope by running water, or weakening of the slope by water saturation from snowmelt or heavy rains. The shaking of the ground by earthquakes or volcanic activity can often trigger landslides. ...
Large igneous province
A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.