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... The Earth formed 4.57 billion years ago out of debris left over from the explosion of a giant star. The Earth began to form as star debris spun round the newly formed Sun and clumped into rocks called planetesimals. Planetesimals were pulled together by their own gravity to form planets such as Ear ...
... The Earth formed 4.57 billion years ago out of debris left over from the explosion of a giant star. The Earth began to form as star debris spun round the newly formed Sun and clumped into rocks called planetesimals. Planetesimals were pulled together by their own gravity to form planets such as Ear ...
Light: The Cosmic Messenger
... shows it is usually quite young • Ocean crust young <200 million years and continental crust much older. ...
... shows it is usually quite young • Ocean crust young <200 million years and continental crust much older. ...
Document
... Abstract The Iberian Margin is well known as a source of rapidly accumulating sediment that contains a high-fidelity record of millennial-scale climate variability for the late Pleistocene. Nick Shackleton demonstrated that piston cores from this region can be correlated precisely to polar ice cores ...
... Abstract The Iberian Margin is well known as a source of rapidly accumulating sediment that contains a high-fidelity record of millennial-scale climate variability for the late Pleistocene. Nick Shackleton demonstrated that piston cores from this region can be correlated precisely to polar ice cores ...
Chapter 9 Planetary Geology: Agenda Ad Hoc Rover Update
... • Our goals for learning • What processes shape planetary surfaces? • Why do the terrestrial planets have different geological histories? • How does a planet’s surface reveal its geological age? ...
... • Our goals for learning • What processes shape planetary surfaces? • Why do the terrestrial planets have different geological histories? • How does a planet’s surface reveal its geological age? ...
as PDF
... California coast and Eastern Pacific Ocean. Nautilus will spend the first two months in the Gulf of Mexico examining the biological impact of the 2010 Gulf Oil Spill as well as studying the fundamental behavior of hydrocarbon seeps as they disperse in the water column to better predict the impact of ...
... California coast and Eastern Pacific Ocean. Nautilus will spend the first two months in the Gulf of Mexico examining the biological impact of the 2010 Gulf Oil Spill as well as studying the fundamental behavior of hydrocarbon seeps as they disperse in the water column to better predict the impact of ...
2 Review Plate Tectonics l
... Plates move relative to each other at a very slow but con Seven major lithospheric plates Average about 5 centimeters (2 inches) per year Seven or so smaller ones. Cooler, denser slabs of oceanic lithosphere desce Plates are in motion and change in shape and size Largest plate is the Pacific plate ...
... Plates move relative to each other at a very slow but con Seven major lithospheric plates Average about 5 centimeters (2 inches) per year Seven or so smaller ones. Cooler, denser slabs of oceanic lithosphere desce Plates are in motion and change in shape and size Largest plate is the Pacific plate ...
Sound Worksheet
... with-depth. Pressure changes become the prime cause of sound speed variability. Because of the higher pressures below 1,000 m, with little change in temperature and salinity, sound speeds at depths below 1,000 m increase / decrease with increasing depth. 4. Sound speeds tend to increase upward from ...
... with-depth. Pressure changes become the prime cause of sound speed variability. Because of the higher pressures below 1,000 m, with little change in temperature and salinity, sound speeds at depths below 1,000 m increase / decrease with increasing depth. 4. Sound speeds tend to increase upward from ...
Week 9a
... Carbon dioxide dissolved in seawater first reacts with the water molecule (H2O) to form carbonic acid (H2CO3). CO2 + H2O = H2CO3 BUT, not all the CO2 dissolved in seawater reacts to make carbonic acid and therefore seawater contains dissolved gaseous CO2 (as in carbonated soda drinks). Carbonic aci ...
... Carbon dioxide dissolved in seawater first reacts with the water molecule (H2O) to form carbonic acid (H2CO3). CO2 + H2O = H2CO3 BUT, not all the CO2 dissolved in seawater reacts to make carbonic acid and therefore seawater contains dissolved gaseous CO2 (as in carbonated soda drinks). Carbonic aci ...
The Effects of Wind Forcing on Surface Currents on the Continental
... ocean mixing, which again effects nutrient transport and connectivity of reefs and fish populations. They also reflect largely on the transfer of energy between the wind field and the upper ocean, which again will allow for an interpretation of divergence and vorticity within the water column. Consi ...
... ocean mixing, which again effects nutrient transport and connectivity of reefs and fish populations. They also reflect largely on the transfer of energy between the wind field and the upper ocean, which again will allow for an interpretation of divergence and vorticity within the water column. Consi ...
Neritic Zone
... • The shallow water over the continental shelf receives: – Sunlight – Steady supply of nutrients washed from the land into the ocean – The light and nutrients enable large plantlike algae to grow – Large quantities of algae is a food source and shelter for other organisms ...
... • The shallow water over the continental shelf receives: – Sunlight – Steady supply of nutrients washed from the land into the ocean – The light and nutrients enable large plantlike algae to grow – Large quantities of algae is a food source and shelter for other organisms ...
KEY Earth`s Interiors Lab Sheet Student Name(s): Use the labeled
... molten rock. It flows very slowly, like hot asphalt. This layer is made of oxygen, silicon, aluminum, and magnesium. ...
... molten rock. It flows very slowly, like hot asphalt. This layer is made of oxygen, silicon, aluminum, and magnesium. ...
Sea-Floor Spreading - Zion Central Middle School
... the ocean crust as molten material erupts from the mantle spreading out and pushing older rocks to the sides of the crack. New ocean floor is continually added by the process of sea-floor ...
... the ocean crust as molten material erupts from the mantle spreading out and pushing older rocks to the sides of the crack. New ocean floor is continually added by the process of sea-floor ...
Plate Tectonics
... They are created when a mantle plume is super heated by the core and burns through the crust building a volcano In the case of an oceanic hotspot, the plate continues to move and the volcano moves off the hotspot, and becomes inactive and just an island. A new volcano will begin to form on the o ...
... They are created when a mantle plume is super heated by the core and burns through the crust building a volcano In the case of an oceanic hotspot, the plate continues to move and the volcano moves off the hotspot, and becomes inactive and just an island. A new volcano will begin to form on the o ...
Document
... of a three-way split in the crust allowing massive lava flows. The split was caused by an upwelling of magma that broke the crust in three directions and poured out lava over hundreds of square miles of Africa and South America. The rocks of the triple junction, which today is the west central porti ...
... of a three-way split in the crust allowing massive lava flows. The split was caused by an upwelling of magma that broke the crust in three directions and poured out lava over hundreds of square miles of Africa and South America. The rocks of the triple junction, which today is the west central porti ...
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... microbial degradation. It is logical to assume that this material has been carried into the intermediate and deep waters by convective processes and may act as a tracer of ocean circulation and of diagenetic transformations of DOC. CDOM has been detected in the deep ocean (4 1000 m) by fluorescence m ...
... microbial degradation. It is logical to assume that this material has been carried into the intermediate and deep waters by convective processes and may act as a tracer of ocean circulation and of diagenetic transformations of DOC. CDOM has been detected in the deep ocean (4 1000 m) by fluorescence m ...
Core
... • Composition: Molten (liquid) metal that is about 4,700°C (8,500°F) • Thickness: 1,400 miles thick • State of Matter: Composed of the melted metals nickel and iron • Located about 1,800 miles beneath the crust. ...
... • Composition: Molten (liquid) metal that is about 4,700°C (8,500°F) • Thickness: 1,400 miles thick • State of Matter: Composed of the melted metals nickel and iron • Located about 1,800 miles beneath the crust. ...
Seafloor Spreading Lab with Makeup
... Background: In the last few decades, scientists have discovered both age and magnetic patterns in the seafloor, which are evidence for plate tectonics. These patterns show that new seafloor has been forming for millions of years at mid-ocean ridges throughout the oceans. Magma melted within the crus ...
... Background: In the last few decades, scientists have discovered both age and magnetic patterns in the seafloor, which are evidence for plate tectonics. These patterns show that new seafloor has been forming for millions of years at mid-ocean ridges throughout the oceans. Magma melted within the crus ...
The E.S.S Project - Laconia School District
... to all of those continents, and that is that at one time all of those continents were once together. • This planet flourished in those five continents over 250 million years ago. • The glossopteris evidence isn't the only evidence that we have to prove that plate tectonics works. • There are mountai ...
... to all of those continents, and that is that at one time all of those continents were once together. • This planet flourished in those five continents over 250 million years ago. • The glossopteris evidence isn't the only evidence that we have to prove that plate tectonics works. • There are mountai ...
Plate Tectonics: Types of Plate Margins
... One with two smaller continents Indo-Australian And one that’s all ocean Pacific ...
... One with two smaller continents Indo-Australian And one that’s all ocean Pacific ...
plate tectonics - Middletown High School
... Plates are made up of the crust and a part of the upper mantle: Lithosphere- Rigid. Made up of crust and upper mantle. 0-100 km thick. Asthenosphere- The plastic-like layer that lies below the lithosphere. ...
... Plates are made up of the crust and a part of the upper mantle: Lithosphere- Rigid. Made up of crust and upper mantle. 0-100 km thick. Asthenosphere- The plastic-like layer that lies below the lithosphere. ...
Geological time scale is hierarchical
... • The widths of alternating magnetic stripes on the opposite sides of a ridge are often roughly symmetrical, and the stripes are generally parallel to the long axis of the ridge. • The banding pattern of any one ocean closely matches that of the others, and the ocean patterns correspond approximatel ...
... • The widths of alternating magnetic stripes on the opposite sides of a ridge are often roughly symmetrical, and the stripes are generally parallel to the long axis of the ridge. • The banding pattern of any one ocean closely matches that of the others, and the ocean patterns correspond approximatel ...
Earth’s Interior PowerPoint - Marcia's Science Teaching
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Ocean
An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.