East Pacific Rise
... LA JOLLA, California--A small group of scientists working in half a dozen different fields here are fitting together bits of evidence to form a picture of a great physical feature of the earth's surface that was all but unknown ten years ago and still might be so had it not been for the Internationa ...
... LA JOLLA, California--A small group of scientists working in half a dozen different fields here are fitting together bits of evidence to form a picture of a great physical feature of the earth's surface that was all but unknown ten years ago and still might be so had it not been for the Internationa ...
Visualization of Ocean Currents and Eddies in a High
... a changing climate. The ocean absorbs carbon dioxide from the atmosphere, influencing the rate of atmospheric warming. The amount of carbon dioxide removed from the atmosphere depends on ocean dynamics, chemistry, and biology. Ocean currents, in turn, transport heat, nutrients and biological constit ...
... a changing climate. The ocean absorbs carbon dioxide from the atmosphere, influencing the rate of atmospheric warming. The amount of carbon dioxide removed from the atmosphere depends on ocean dynamics, chemistry, and biology. Ocean currents, in turn, transport heat, nutrients and biological constit ...
Essential Questions - Thomas C. Cario Middle School
... P-waves: Move back and forth parallel to the direction of the wave (slinky), fastest wave, and can travel through liquids and solids. S-waves: Move at right angles to the direction of the wave (rope), 2nd fastest wave, and cannot travel through liquid, only solid. Surface waves: Slowest wave and cau ...
... P-waves: Move back and forth parallel to the direction of the wave (slinky), fastest wave, and can travel through liquids and solids. S-waves: Move at right angles to the direction of the wave (rope), 2nd fastest wave, and cannot travel through liquid, only solid. Surface waves: Slowest wave and cau ...
x3 x3 x3 x3 x3 x3 x3 x3 x3 x3 x3 x3 x3 x3 x3 x3
... ocean basins. Plate tectonics says that ocean crust moves too – the whole surface of the earth is broken into plates which ...
... ocean basins. Plate tectonics says that ocean crust moves too – the whole surface of the earth is broken into plates which ...
INSIDE THE EARTH
... convection currents. The mantle that is close to the core heats up and rises, mantle that is away cools down and sinks. This just keeps happening to create a current. ...
... convection currents. The mantle that is close to the core heats up and rises, mantle that is away cools down and sinks. This just keeps happening to create a current. ...
Emma Wilson Extra Credit #3 Unit 1: 1. Which of the following does
... B. Science keeps track of what works and what doesn’t. C. Science assumes theories are correct based off of the hypothesis. D. Science tests the structure of knowledge continually. Science is tested against reality. Science requires observation AND experimentation to prove something. A hypothesis is ...
... B. Science keeps track of what works and what doesn’t. C. Science assumes theories are correct based off of the hypothesis. D. Science tests the structure of knowledge continually. Science is tested against reality. Science requires observation AND experimentation to prove something. A hypothesis is ...
1 IDS 102 Plate Tectonics Questions Part I: Observations
... Part I: Observations- Four maps of world are positioned around the room. Answer the questions associated with each map and record your general observations about the maps. World topography- this map portrays the elevation of the Earth’s surface by color. See the scale along the side of the map for t ...
... Part I: Observations- Four maps of world are positioned around the room. Answer the questions associated with each map and record your general observations about the maps. World topography- this map portrays the elevation of the Earth’s surface by color. See the scale along the side of the map for t ...
Bodies of Water Notes - Raleigh Charter High School
... i. Lies between Iceland and Norway and is separated from the Atlantic by the Faeroe-Iceland Ridge ii. Kept free of ice by the warm North Atlantic Drift the flows from Scotland Baltic Sea i. Shallow enclosed inland sea with little tide and branches out into Gulf of Bothnia and Gulf of Finland. ii. It ...
... i. Lies between Iceland and Norway and is separated from the Atlantic by the Faeroe-Iceland Ridge ii. Kept free of ice by the warm North Atlantic Drift the flows from Scotland Baltic Sea i. Shallow enclosed inland sea with little tide and branches out into Gulf of Bothnia and Gulf of Finland. ii. It ...
Introduction to Plate Tectonics
... – a great mountain range on the ocean floor, the global mid-ocean ridge, encircled the Earth. • more than 50,000 kilometers (km) long and up to 1000 km across • zig-zags between the continents • Rising about 4,500 meters(m) above the sea floor, – Taller than all mountains in the US except for Mount ...
... – a great mountain range on the ocean floor, the global mid-ocean ridge, encircled the Earth. • more than 50,000 kilometers (km) long and up to 1000 km across • zig-zags between the continents • Rising about 4,500 meters(m) above the sea floor, – Taller than all mountains in the US except for Mount ...
Internal Structure of the Earth
... • Using ________ waves, they can tell whether an object is a _____ or a _____, so by using that information, they theorized about the interior layers of the Earth ...
... • Using ________ waves, they can tell whether an object is a _____ or a _____, so by using that information, they theorized about the interior layers of the Earth ...
Plate Tectonics
... cracked shell of an egg •the pieces of the shell are Earth's tectonic plates -- there are 12 major ones -- and they float along on vast convection currents in the asthenosphere •the asthenosphere churns like a fluid ...
... cracked shell of an egg •the pieces of the shell are Earth's tectonic plates -- there are 12 major ones -- and they float along on vast convection currents in the asthenosphere •the asthenosphere churns like a fluid ...
I-6 Dynamic Planet Notes
... supercontinents. One may have existed about 600 million years ago. At the time of Pangea, the Pacific Ocean was the only ocean! (Pacific Ocean is surrounded by subduction zones and is being consumed ...
... supercontinents. One may have existed about 600 million years ago. At the time of Pangea, the Pacific Ocean was the only ocean! (Pacific Ocean is surrounded by subduction zones and is being consumed ...
Chapter 1
... Supports tourism Some marine organisms cause problems by causing disease or attacking people ...
... Supports tourism Some marine organisms cause problems by causing disease or attacking people ...
Climate Matters at Scripps - Scripps Institution of Oceanography
... faces massive changes in weather patterns, sea levels, ocean acidity, and oxygen levels. As already seen in events such as Superstorm Sandy and record-breaking droughts, climate change is in motion. If societies do not respond, their populations face water and food shortages and severe economic disr ...
... faces massive changes in weather patterns, sea levels, ocean acidity, and oxygen levels. As already seen in events such as Superstorm Sandy and record-breaking droughts, climate change is in motion. If societies do not respond, their populations face water and food shortages and severe economic disr ...
Bathymetry_Activity
... Part 3: Exploring the Sea Floor: The Deep Ocean The deep-sea floor, between 4000 m and 6000 m, covers 30% of the Earth’s surface and is composed primarily of large flat plains extending from the base of the continental slope which are broken up by ridges, rises, fracture zones, and seamounts. These ...
... Part 3: Exploring the Sea Floor: The Deep Ocean The deep-sea floor, between 4000 m and 6000 m, covers 30% of the Earth’s surface and is composed primarily of large flat plains extending from the base of the continental slope which are broken up by ridges, rises, fracture zones, and seamounts. These ...
outcome highlights
... IO Net is an international collaborative network for the organisations and individuals (called “Partners”) who support the Joint Policy Recommendations “For the Better Conservation and Management of Islands and Their Surrounding Ocean Areas” and collaborate and cooperate on a voluntary basis to impl ...
... IO Net is an international collaborative network for the organisations and individuals (called “Partners”) who support the Joint Policy Recommendations “For the Better Conservation and Management of Islands and Their Surrounding Ocean Areas” and collaborate and cooperate on a voluntary basis to impl ...
EESS 8: The Oceans Activity 2 The Shape of Ocean Basins and the
... Part 3: Exploring the Sea Floor: The Deep Ocean The deep-sea floor, between 4000 m and 6000 m, covers 30% of the Earth’s surface and is composed primarily of large flat plains extending from the base of the continental slope which are broken up by ridges, rises, fracture zones, and seamounts. These ...
... Part 3: Exploring the Sea Floor: The Deep Ocean The deep-sea floor, between 4000 m and 6000 m, covers 30% of the Earth’s surface and is composed primarily of large flat plains extending from the base of the continental slope which are broken up by ridges, rises, fracture zones, and seamounts. These ...
1. What causes Earth`s precession or earth`s wobbling?
... 21. What will eventually happen when the crust along the boundary becomes so thin? _____________________________________________________________________________________ _____________________________________________________________________________________ 22. How did Saudi Arabia get torn away from A ...
... 21. What will eventually happen when the crust along the boundary becomes so thin? _____________________________________________________________________________________ _____________________________________________________________________________________ 22. How did Saudi Arabia get torn away from A ...
pdf - University of California, Berkeley
... But the Juan de Fuca plate was itself young at the time (there's a mid-ocean ridge just off the coast of Oregon that forms brand new crust to this day), so it hadn't had the chance fully harden yet. When the crust and hot spot met, the hot mantle plume to found a weakness in the plate -- perhaps a p ...
... But the Juan de Fuca plate was itself young at the time (there's a mid-ocean ridge just off the coast of Oregon that forms brand new crust to this day), so it hadn't had the chance fully harden yet. When the crust and hot spot met, the hot mantle plume to found a weakness in the plate -- perhaps a p ...
amazonbasingeologicaldevelopment
... • Matching rocks and fossils in Eastern South America and Western Africa; • Matching coastline shapes; • Magnetic “stripes” on Atlantic sea-floor rocks on either side of the Mid-Atlantic Ridge Water ran off the continent to the west, depositing sediments into the Pacific Ocean ...
... • Matching rocks and fossils in Eastern South America and Western Africa; • Matching coastline shapes; • Magnetic “stripes” on Atlantic sea-floor rocks on either side of the Mid-Atlantic Ridge Water ran off the continent to the west, depositing sediments into the Pacific Ocean ...
ES2 Sea floor spreading Name: Introduction: About 30 years ago
... the magnetic field of the Earth. Rocks forming today point North, but at times in the past they pointed South. On either side of the midocean ridge is a mirror image of magnetic patterns and ages of rock. This gave evidence for Sea Floor spreading and plate tectonics. While new crust is created at d ...
... the magnetic field of the Earth. Rocks forming today point North, but at times in the past they pointed South. On either side of the midocean ridge is a mirror image of magnetic patterns and ages of rock. This gave evidence for Sea Floor spreading and plate tectonics. While new crust is created at d ...
the proof-----seafloor spreading
... THE PROOF-----SEAFLOOR SPREADING •An American scientist named Harry Hess proposed the seafloor spreading theory in ...
... THE PROOF-----SEAFLOOR SPREADING •An American scientist named Harry Hess proposed the seafloor spreading theory in ...
Slide 1
... The Theory of Plate Tectonics Slip-Sliding Away In 30 million years, this airplane might take one hour longer to fly from Florida to London than it takes today. That’s because Florida and Europe are riding on two different pieces of Earth’s crust that are moving slowly away from each other! ...
... The Theory of Plate Tectonics Slip-Sliding Away In 30 million years, this airplane might take one hour longer to fly from Florida to London than it takes today. That’s because Florida and Europe are riding on two different pieces of Earth’s crust that are moving slowly away from each other! ...
Week 3 (Norton), part b (pdf, 5.7 MB)
... One of the most vexing problems late in the process of Global Tectonic Theory’s acceptance was the realization that there was a type of fault previously unrecognized by earth scientists, transform faults, that transected roughly perpendicularly mid ocean ridges. A couple of papers by Tuzo Wilson, a ...
... One of the most vexing problems late in the process of Global Tectonic Theory’s acceptance was the realization that there was a type of fault previously unrecognized by earth scientists, transform faults, that transected roughly perpendicularly mid ocean ridges. A couple of papers by Tuzo Wilson, a ...
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.