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This Dynamic Earth [USGS]
This Dynamic Earth [USGS]

... Harry Hess (1906-1969) in his Navy uniform as Captain of the assault transport Cape Johnson during World War II. After the war, he remained active in the Naval Reserve, reaching the rank of Rear Admiral. (Photograph courtesy of Department of Geological and Geophysical Sciences, Princeton University. ...
December 26, 2004 Indian Ocean Earthquake & Tsunami
December 26, 2004 Indian Ocean Earthquake & Tsunami

... • From the Japanese word tsunami meaning "harbor wave“ • Often mistakenly called "tidal waves“. • They have nothing to do with tidal action. • Seismic sea waves caused by earthquakes, submarine landslides, and, infrequently, by eruptions of island volcanoes. ...
convergent boundary
convergent boundary

... But the purpose of the Glomar Challenger was scientific exploration. One of the most important discoveries was made during Leg 3. The crew drilled 17 holes at 10 different sites along a oceanic ridge between South America and Africa. The core samples retrieved provided definitive proof for continent ...
Fact Sheet - SharpSchool
Fact Sheet - SharpSchool

... stated that Pangaea started breaking up about 200 million years ago and the pieces began moving into their current location. The big reason that people didn’t believe this theory was because there because Wegner had no evidence to prove what force caused the continents to move and Wegner did try to ...
unit 2 earth history lecture and study guide
unit 2 earth history lecture and study guide

... 1) The sea floor is divided by a large ridge (mountain) system that extends almost 40,000 miles in length and is about 900 miles wide. 2) This ridge system is continuous around Earth’s entire globe. 3) The mountains at the center of the ocean are much higher than the distant abyssal plain found towa ...
Demonstrating Archimedes` Principle
Demonstrating Archimedes` Principle

... comes in two flavors: continental crust varies in thickness, averaging about 35 km, and has a heterogeneous composition which, on average, resembles granite (silicate-based rocks rich in sodium, potassium and aluminum); oceanic crust is much thinner, typically 8-10 km thick, and is composed of basal ...
• The ridges and trenches on the ocean bottom cause corresponding
• The ridges and trenches on the ocean bottom cause corresponding

... where farther west, so this ridge was left behind to sub­ side," explains Haxby. But it continues to rest on the sea bottom as a vital piece of evidence that will help research­ ers trace the evolution of the oceans, a process crucial to the development of climatic patterns. Such revelations in the ...
oceans, seafloor, and continental margins
oceans, seafloor, and continental margins

... • Seamounts and guyots are common,  widespread features of the sea floor.  • Seamounts rise more than a kilometer from  the ocean floor and are remnants of oceanic  ridge volcanoes; Guyots have the same origin  but are flat‐topped .  • Aseismic ridges consisting of seamounts and guyots extend in a p ...
Microsoft PowerPoint - file.in [jen pro \350ten\355]
Microsoft PowerPoint - file.in [jen pro \350ten\355]

... In 1980 Walter and Luis Alvarez and their colleagues Frank Asaro and Helen Michel published an historic paper suggesting that an asteroid about 10 kilometers (6 miles) in diameter struck the earth sixty-five million years ago at the end of the Cretaceous. The resulting impact should have left a cra ...
Plate Tectonics
Plate Tectonics

... 2.) What is the evidence that supports continental drift? 3.) Why would you expect to see similar rocks and rock structures on two landmasses that were connected at one time? ...
Chapter 1: INTRODUCTION
Chapter 1: INTRODUCTION

... tracks (315 km at the equator) may result in non-homogeneity while presenting a composite of larger area (Rosmorduc et al., 2011). Due to its low temporal resolution (10 day ground track repeated cycle), it is not suitable for short time scale event such as daily variations. ...
Sea Monsters - The Barr Bunch
Sea Monsters - The Barr Bunch

... school bus. Many glow in the dark. Most have razor-sharp teeth. And we're just beginning to discover more of them. Few places on our planet are as mysterious as the deep sea. Until recently, scientists doubted that many creatures could live there. Now experts are taking a deeper look at the ocean. S ...
triple junction
triple junction

... India began to collide with Asia forming the Himalayan Mountain Range (Oligocene to Recent) Africa started to shift northward, gradually sliding under Europe and uplifting the Alps (Oligocene to Recent) Continued westward movement of North America and South America formed an on again off again la ...
File
File

... – outermost layer – thinnest layer – the layer we live on – divided into pieces, called tectonic plates – two types: continental and oceanic crust Mantle – thickest layer – “flows” and allows the tectonic plates to move on top – primarily magma ...
Plate Boundaries Lithospheric plates move as coherent units
Plate Boundaries Lithospheric plates move as coherent units

... square kilometers of new seafloor. This mechanism has created the floor of the Atlantic Ocean during the past 160 million years and is appropriately called seafloor spreading. Because seafloor spreading is the dominant process associated with divergent boundaries, these zones are sometimes referred ...
Lecture#3 part1: Dynamic Earth
Lecture#3 part1: Dynamic Earth

... • So, continents are no longer thought to plow through oceanic crust • Continents are part of plates that move on the soft, plastic asthenosphere. • driving force: convection currents ...
Input to the Decadal Survey Inner Planets Panel Mission Concept
Input to the Decadal Survey Inner Planets Panel Mission Concept

... A capable surface lander could address a majority of the key questions about the evolution of Venus. The increasing recognition of the interaction between volatiles, the interior and climate evolution as modulated by geology and tectonics (Phillips et al., 2001; Smrekar et al., 2007; Lenardic et al. ...
Ch 13 MORB mod 9
Ch 13 MORB mod 9

... There are incompatible-rich and incompatible-poor mantle source regions for MORB magmas – N-MORB (normal MORB) taps the depleted upper mantle source  Mg# > 65: K2O < 0.10 TiO2 < 1.0  Depleted in LREE, Low LILE e.g. K+ – E-MORB (enriched MORB, also called P-MORB for plume) taps the (deeper) fertil ...
Slide 1
Slide 1

... • BR: How do you think you did on the test yesterday? ...
Essential Oceanography
Essential Oceanography

... Squid are considered meroplankton (opposite = holoplankton) “mero” – part “holo” - whole ...
Light: The Cosmic Messenger
Light: The Cosmic Messenger

... shows it is usually quite young • Ocean crust young <200 million years and continental crust much older. ...
Classification of living things
Classification of living things

... and nektonic stages Squid are considered meroplankton (opposite = holoplankton) Figure 12-3 ...
Right Side Crust
Right Side Crust

... Turn on the “Seafloor age” and the “Plate Boundary” Google Earth (GE) layers. The “Seafloor age” layer shows the ages of volcanic rocks that have erupted and cooled to form the ocean floor. Focus on the Atlantic Ocean. Note that the age bands generally run parallel to the spreading ridges. Seafloor ...
Word
Word

... A. the Earth is comprised of many layers with different densities B. the deep interior of the Earth must have a density greater than 5.5 g/cm 3 C. the deep interior of the Earth must have a density less than 5.5 g/cm 3 D. the deep interior of the Earth must have a density less than 2.5 g/cm3 E. meas ...
distribution of oceans and continents
distribution of oceans and continents

... oceanic lithosphere. Plates move horizontally over the asthenosphere as rigid units. The lithosphere includes the crust and top mantle with its thickness range varying between 5-100 km in oceanic parts and about 200 km in the continental areas. A plate may be referred to as the continental plate or ...
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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.
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