• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Plate Tectonics Crossword
Plate Tectonics Crossword

... the planet Earth. 8. The outer part of the Earth's crust. It is composed of solid rock. ...
The Physical World
The Physical World

... All people, animals and plants that live on or close to the earths surface. The part of earth that supports life is called the biosphere. ...
Global phosphorus cycle
Global phosphorus cycle

...  Cd:Ca ratio in benthic forams as a proxy for DIP  [Cd] is linearly correlated to [PO4] (DIP) in modern oceans. ...
Orogenies as records of plate collisions
Orogenies as records of plate collisions

... the ocean crust-bearing plate of on the right, but later it is the ocean-bearing plate on the left. The controlling factor? The more dense plate will subduct. ...
Plate Tectonics – A Geologic Revolution
Plate Tectonics – A Geologic Revolution

... as one moved across the ocean basin. This variation was more or less symmetrically distributed around mid-ocean ridge systems. How might this happen? ...
Chapter 15 - Life Near the Surface
Chapter 15 - Life Near the Surface

... Another way to stay afloat is by storing ________________________. Many bony fish do this through an organ called a _____________________ ____________________. Fish can then adjust their position in the water column by changing ____________________________________________________________. Not all pl ...
The last frontier on Earth - Centre for International Law
The last frontier on Earth - Centre for International Law

... know less about ocean space than we do about outer space. On March 26 last year, the awardwinning American movie director, James Cameron, descended alone in a submersible called the "Deepsea Challenger" to the bottom of the Mariana Trench. It is the deepest part of the ocean floor at 11km below the ...
plate tectonics
plate tectonics

... PROVE HIS CONTINENTAL DRIFT THEORY: 1) _______________________________________________________________ 2) _______________________________________________________________ 3) _______________________________________________________________ 4) ____________________________________________________________ ...
Ophiolite_ppt_presentation
Ophiolite_ppt_presentation

... plates in ocean setting. The particular type of plate boundary that yields island arcs is called subduction zone. • Fore-arc basin – located to the “front” of the volcanic arc; forms toward the subducted plate side. • Back-arc basin – associated with island arc and subduction zone; found at converge ...
Nutrient Cycles
Nutrient Cycles

... Demonstrate an understanding that the reservoir of dissolved nutrients is depleted by uptake into organisms in food chains. • One of the ways in which nutrients are removed from the surface waters of an ocean is by their uptake by primary producers, (phytoplankton) and their use for the synthesis ...
March 27th Scientist`s Walk on the Wildside: Campers take a
March 27th Scientist`s Walk on the Wildside: Campers take a

... Creatures of the Deep: Campers will identify the five layers of the ocean, from the Sunlight zone (0-600 feet) all the way down to the abyss and the deep trenches (36,000 feet below the surface). They will see examples of creatures and fish which can survive in the harsh depths of the ocean. Campers ...
OCEANS: EARTH`S LAST FRONTIER
OCEANS: EARTH`S LAST FRONTIER

... about what goes on in the oceans, but argues that it is not necessary to be a scientist to explore them. The scene shifts to the schooner Phoenix, part of the Coastal Ecology Learning Program on Long Island Sound. The video shows students aboard the Phoenix measuring the salinity of seawater, and t ...
AP Chapter 5 Study Guide - Bennatti
AP Chapter 5 Study Guide - Bennatti

... Albedo- the proportional reflectance of Earth’s surface; glaciers and ice sheets have high albedos and reflect most of the sunlight hitting their surfaces while oceans and forests have low albedos Coriolois effect- the tendency of moving air or water to be deflected from its path to the right in the ...
Study Guide
Study Guide

... b. similar fossils on different land masses c. similar rock types and structures on different land masses d. similar evidence of ancient climates on different land masses 2. One of the main objections to Wegener’s continental drift hypothesis was his inability to provide a mechanism that was capable ...
Chapter 2
Chapter 2

... The Indian Ocean: Relict Species What is this fish? ...
germany`s new research center for marine geosciences (geomar)
germany`s new research center for marine geosciences (geomar)

... located on a fjord open to the western Baltic Sea, with easy access for research ships of all nations. G E O M A R has a 500m-long dock suitable for most ocean-going research vessels. The Technology Park will be located directly across the l]ord from the Institut fiir Meereskunde and the University. ...
Mid-Term exam Study Guide KEY link
Mid-Term exam Study Guide KEY link

... 42) What will you usually find in areas of low pressure? cloudy weather. 43) Why do high pressure areas usually have good weather? the air masses sink, making it difficult for clouds to form ...
Activity Title: Introduction to Ocean Zones
Activity Title: Introduction to Ocean Zones

... What is the photic zone and how does it compare in size to the other ocean zones? (The top 10 m is where most visible light occurs and then decreases in quality and quantity down to 200m. It is a very tiny fraction of the depths of the open ocean). ...
The Growth of Marine Labs
The Growth of Marine Labs

... data by precise instruments effected by heavy waves. ...
Take Home 12 Complete the following on your own paper. Do not
Take Home 12 Complete the following on your own paper. Do not

... increases in density and sinks. Science Student 3: Magma in the mantle is moved by convection. It is theorized that the internal heat of the earth causes the magma to rise to the top of the mantle. As it rises, it cools, density increases and the magma sinks again towards the core. Which of the foll ...
Environmental Problems
Environmental Problems

... ocean surface waters – Melting of land glaciers and ice caps – Thermal expansion of deep-ocean waters © 2011 Pearson Education, Inc. ...
Chapter 2
Chapter 2

...  Faults are formed from this process  Earthquakes are produced from this process ...
LAB 4-3: Seafloor Spreading
LAB 4-3: Seafloor Spreading

... slope, a steep downward slope where ocean depth increases dramatically. The base of this slope represents the boundary between continental and oceanic crust. Beyond the continental slope consists of a vast, flat area of the deep-ocean basin called an abyssal plain. Abyssal plains are the flattest re ...
Seafloor spreading and recycling of oceanic crust
Seafloor spreading and recycling of oceanic crust

... the oceanic ridges. If the Earth's crust was expanding along the oceanic ridges, Hess reasoned, it must be shrinking elsewhere. He suggested that new oceanic crust continuously spread away from the ridges in a conveyor belt-like motion. Many millions of years later, the oceanic crust eventually desc ...
The Ocean Floor - Travelling across time
The Ocean Floor - Travelling across time

... The Ocean Floor In the following diagram there is evidence of seafloor spreading by showing the ages of the ocean floor. The red colors are the youngest parts of the seafloor, where fresh new crust is formed as lava seeps up from the deep interior of the Earth at spreading ridges. The green colors ...
< 1 ... 158 159 160 161 162 163 164 165 166 ... 220 >

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.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report