 
									
								
									earth*s internal processes
									
... similar to waves that travel along a coiled spring. Primary waves cause particles inside the Earth to move back and forth in the same direction that the wave is traveling. P-waves are faster seismic waves and can travel through Earth’s interior with speeds between 5 km/s and 7 km/s. P-waves travel t ...
                        	... similar to waves that travel along a coiled spring. Primary waves cause particles inside the Earth to move back and forth in the same direction that the wave is traveling. P-waves are faster seismic waves and can travel through Earth’s interior with speeds between 5 km/s and 7 km/s. P-waves travel t ...
									5 layer density model
									
... Background: Density is a concept that you will hear and that we will cover frequently in Earth science. Many of the movements of substances on Earth are due to their density. In this investigation you will be testing the densities of 5 different liquids to determine which is the most and which is th ...
                        	... Background: Density is a concept that you will hear and that we will cover frequently in Earth science. Many of the movements of substances on Earth are due to their density. In this investigation you will be testing the densities of 5 different liquids to determine which is the most and which is th ...
									Geological Processes class Booklet
									
...  He was unable to convincingly explain how the continents could move  The current theory of plate tectonics became widely accepted in the 1960’s, by which time other scientists had found evidence to show that it is the Earth’s plates that move and that they do so as a result of convection currents ...
                        	...  He was unable to convincingly explain how the continents could move  The current theory of plate tectonics became widely accepted in the 1960’s, by which time other scientists had found evidence to show that it is the Earth’s plates that move and that they do so as a result of convection currents ...
									plate tectonics notes File
									
... layer of the Earth, the lithosphere, is composed of several rigid, large plates that move relative to one another by sliding on a weak layer, the asthenosphere in the upper mantle; continents and ocean basins are passive riders on these plates. This is a unifying concept of geology developed after W ...
                        	... layer of the Earth, the lithosphere, is composed of several rigid, large plates that move relative to one another by sliding on a weak layer, the asthenosphere in the upper mantle; continents and ocean basins are passive riders on these plates. This is a unifying concept of geology developed after W ...
									Volcano ppt notes
									
...  The most common type of eruption  Produces relatively calm flows of lava  Found in much of the seafloor, Northwest regions of the US, & other vast regions on Earth’s surface  Examples: Mauna Loa & Kilauea in Hawaii ...
                        	...  The most common type of eruption  Produces relatively calm flows of lava  Found in much of the seafloor, Northwest regions of the US, & other vast regions on Earth’s surface  Examples: Mauna Loa & Kilauea in Hawaii ...
									Metamorphic Rock
									
... Colliding Continental Plates  Mountain ranges are created where Collisions between ...
                        	... Colliding Continental Plates  Mountain ranges are created where Collisions between ...
									3_Earthquakes
									
... B) Surface Waves—created when body waves poke out at Earth’s surface; can only travel along Earth’s surface (like ocean waves). A) Body Waves: P-waves & S-waves 1) P-Waves— “P” for ‘primary’ arrive first, travel fastest through rock; made up of alternating compressions and dilations; move rock part ...
                        	... B) Surface Waves—created when body waves poke out at Earth’s surface; can only travel along Earth’s surface (like ocean waves). A) Body Waves: P-waves & S-waves 1) P-Waves— “P” for ‘primary’ arrive first, travel fastest through rock; made up of alternating compressions and dilations; move rock part ...
									Plate Tectonics
									
... “Subduction”.In this process continental plate forced on oceanic plate to subduct. When oceanic crust enters into mantle it starts floating backward,in other words magma erupts and Volcanoes created. ...
                        	... “Subduction”.In this process continental plate forced on oceanic plate to subduct. When oceanic crust enters into mantle it starts floating backward,in other words magma erupts and Volcanoes created. ...
									PowerPoint Presentation - The Earth, Plate Tectonics
									
... Convection is like a boiling pot. Heated soup rises to the surface, spreads and begins to cool, and then sinks back to the bottom of the pot where it is reheated and rises again. ...
                        	... Convection is like a boiling pot. Heated soup rises to the surface, spreads and begins to cool, and then sinks back to the bottom of the pot where it is reheated and rises again. ...
									Continental Drift Theory
									
... • First proposed by Alfred Wegener in 1912: – 250 million years ago, all of the continents were combined into one super-continent called “Pangaea” – The continents gradually drifted apart to where they are today ...
                        	... • First proposed by Alfred Wegener in 1912: – 250 million years ago, all of the continents were combined into one super-continent called “Pangaea” – The continents gradually drifted apart to where they are today ...
									File
									
... that measures the ground’s movements. (21)Other meters, such as the strainmeter and tiltmeter, measure changes in Earth’s crust. (22)Lasers are used to detect small movements across fault lines. (23)A scale called the Richter scale measures the force of an earthquake. (24)Scientists can learn about ...
                        	... that measures the ground’s movements. (21)Other meters, such as the strainmeter and tiltmeter, measure changes in Earth’s crust. (22)Lasers are used to detect small movements across fault lines. (23)A scale called the Richter scale measures the force of an earthquake. (24)Scientists can learn about ...
									Chapter 22 Vocabulary ReviewA Directions: Complete this sheet
									
... Type of seismic wave that travels by expanding and compressing (like an accordion) Type of seismic wave that causes the most damage to structures (also the slowest) Type of seismic wave that travels by vibrating crust up and down while moving forward (like a snake) __________________ Type of seismic ...
                        	... Type of seismic wave that travels by expanding and compressing (like an accordion) Type of seismic wave that causes the most damage to structures (also the slowest) Type of seismic wave that travels by vibrating crust up and down while moving forward (like a snake) __________________ Type of seismic ...
									Earth Layers Review
									
... Directions: Write the name of the correct layer in the box next to the description This layer is a solid ball of iron and nickel. ...
                        	... Directions: Write the name of the correct layer in the box next to the description This layer is a solid ball of iron and nickel. ...
									earth-_ch_6_tectonic_plates_study_guide
									
... 14. What type of boundary is formed when plates slide past each other? 15. According to the continental drift theory, a single, huge continent once existed called TECs1.3.1 16. What type of boundary is formed when plates separate? ...
                        	... 14. What type of boundary is formed when plates slide past each other? 15. According to the continental drift theory, a single, huge continent once existed called TECs1.3.1 16. What type of boundary is formed when plates separate? ...
									Earth Communication
									
... In the late 1950's, scientists mapped the present-day magnetic field generated by rocks on the floor of the Pacific Ocean. The volcanic rocks that make up the sea floor have magnetization because, as they cool, magnetic minerals within the rock align to the Earth's magnetic field. The intensity of t ...
                        	... In the late 1950's, scientists mapped the present-day magnetic field generated by rocks on the floor of the Pacific Ocean. The volcanic rocks that make up the sea floor have magnetization because, as they cool, magnetic minerals within the rock align to the Earth's magnetic field. The intensity of t ...
									Earth Communication
									
... In the late 1950's, scientists mapped the present-day magnetic field generated by rocks on the floor of the Pacific Ocean. The volcanic rocks that make up the sea floor have magnetization because, as they cool, magnetic minerals within the rock align to the Earth's magnetic field. The intensity of ...
                        	... In the late 1950's, scientists mapped the present-day magnetic field generated by rocks on the floor of the Pacific Ocean. The volcanic rocks that make up the sea floor have magnetization because, as they cool, magnetic minerals within the rock align to the Earth's magnetic field. The intensity of ...
									plate tectonics webquest
									
... Earth. Define the layers of the Earth and draw a diagram which includes all of the layers. Crust ...
                        	... Earth. Define the layers of the Earth and draw a diagram which includes all of the layers. Crust ...
									plate tectonics
									
... Transform boundaries, where plates slide past each other. Tectonic plates have irregular edges. They grind and jerk as they slide, which produces earthquakes. We can determine the time and location of earthquakes by using a seismograph which locates the epicenter. The point on the Earth’s surface di ...
                        	... Transform boundaries, where plates slide past each other. Tectonic plates have irregular edges. They grind and jerk as they slide, which produces earthquakes. We can determine the time and location of earthquakes by using a seismograph which locates the epicenter. The point on the Earth’s surface di ...
									plate tectonics - University of Alaska Fairbanks
									
... Office hours: After class, Tuesday/Thursday 2:00-3:00, or by appointment Textbook: Tectonics, Eldridge M. Moores and Robert J. Twiss, W.H. Freeman & Co., New York, 415 p., 1995 The concept that rigid lithospheric plates move relative to one another and interact at their boundaries has revolutionized ...
                        	... Office hours: After class, Tuesday/Thursday 2:00-3:00, or by appointment Textbook: Tectonics, Eldridge M. Moores and Robert J. Twiss, W.H. Freeman & Co., New York, 415 p., 1995 The concept that rigid lithospheric plates move relative to one another and interact at their boundaries has revolutionized ...
									PLATE TECTONICS He thought that continents were an only piece
									
... • Transform boundaries: the San Andreas Fault zone in California, that it connects the East Pacific Rise with the South Gord. Plate tectonic and ocean trenches have in common the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate called s ...
                        	... • Transform boundaries: the San Andreas Fault zone in California, that it connects the East Pacific Rise with the South Gord. Plate tectonic and ocean trenches have in common the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate called s ...
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.
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									