Continental Drift and Plate Tectonics
... 1. Continental Plate to Continental Plate: the two plates just fold together and keep pushing on each other. Mountains are formed. (example: Himalayas) 2. Continental Plate to Ocean Plate: two plates come together and the oceanic plate slides underneath the continental plate. The lower one starts be ...
... 1. Continental Plate to Continental Plate: the two plates just fold together and keep pushing on each other. Mountains are formed. (example: Himalayas) 2. Continental Plate to Ocean Plate: two plates come together and the oceanic plate slides underneath the continental plate. The lower one starts be ...
Notes Rdg Guide Plate Tectonics Pw Pt 2016
... In science & technology Allow scientists to Develop the Theory Of Plate Tectonics ...
... In science & technology Allow scientists to Develop the Theory Of Plate Tectonics ...
WGCh2NotetakingKey
... 2. This type of freshwater comes from rain and snow that has filtered through the soil and rock and accumulated below the Earth’s surface. Some water from lakes and rivers may also become part of the groundwater. 3. People often dig wells and use springs that tap into this type of freshwater. ...
... 2. This type of freshwater comes from rain and snow that has filtered through the soil and rock and accumulated below the Earth’s surface. Some water from lakes and rivers may also become part of the groundwater. 3. People often dig wells and use springs that tap into this type of freshwater. ...
An Educator`s Guide - American Museum of Natural History
... Blue Whale and Open Ocean Ecosystem — The centerpiece of the Hall is a life-size model of the world’s largest animal, the giant blue whale. Text panels on drifters, migrants, ocean exploration, and the food web can be found along the mezzanine rail. An int e ractive on whale research and cons e r v ...
... Blue Whale and Open Ocean Ecosystem — The centerpiece of the Hall is a life-size model of the world’s largest animal, the giant blue whale. Text panels on drifters, migrants, ocean exploration, and the food web can be found along the mezzanine rail. An int e ractive on whale research and cons e r v ...
Magnetic Field, Sea-floor Spreading, Deep
... MAGNETIC FIELD Some of our most important evidence of sea-floor spreading comes from magnetic reversals recorded on the ocean floor The magnetic poles can change place (called magnetic reversal) Magnetic mineral grains line up in opposite direction of magnetic field ...
... MAGNETIC FIELD Some of our most important evidence of sea-floor spreading comes from magnetic reversals recorded on the ocean floor The magnetic poles can change place (called magnetic reversal) Magnetic mineral grains line up in opposite direction of magnetic field ...
Powerpoint for today
... Plates ride on top of convective cells. Lava flows through cell boundaries. Earth loses internal heat this way. ...
... Plates ride on top of convective cells. Lava flows through cell boundaries. Earth loses internal heat this way. ...
RADIOCARBON IN PARTICULATE MATTER FROM THE Woods
... that the trap was free of contaminated particulate carbon that had been fixed at the surface near the dump sites. Besides, if the trap material were contaminated, we would expect both PIG and PUG to contain similar 14C levels, and this was not observed. It is thus difficult to explain the 14C data s ...
... that the trap was free of contaminated particulate carbon that had been fixed at the surface near the dump sites. Besides, if the trap material were contaminated, we would expect both PIG and PUG to contain similar 14C levels, and this was not observed. It is thus difficult to explain the 14C data s ...
Oceanic and Coastal Remote Sensing
... the wearing down of land by erosion, and the redistribution of material by sediment transport and deposition. To measure or detect the ocean is greatly challenging because it changes all the time. As the result of rapid data acquisition and uniform quality of global data set, remote sensing plays an ...
... the wearing down of land by erosion, and the redistribution of material by sediment transport and deposition. To measure or detect the ocean is greatly challenging because it changes all the time. As the result of rapid data acquisition and uniform quality of global data set, remote sensing plays an ...
MarineSediments
... Sedimentation in the Ocean Deep-sea Sedimentation has two main sources of sediment: external- terrigenous material from the land and internal-biogenic and authigenic from the sea. ...
... Sedimentation in the Ocean Deep-sea Sedimentation has two main sources of sediment: external- terrigenous material from the land and internal-biogenic and authigenic from the sea. ...
Review sheet – Oceanography – first midterm
... turbidity current fracture zone hydrothermal vent seamount abyssal plain passive margin active margin ...
... turbidity current fracture zone hydrothermal vent seamount abyssal plain passive margin active margin ...
Study of frontal zones in the crozet-kerguelen region
... The hydrological stations established in spring (November 1972) along 70°E reveal at 46°S the northern limit of the 2°C isotherm and the presence of two fronts at 46 and 43°S, separated, from the surface to 300 rn, by · a relatively homogeneous water (temperature about 9°C, salinity about 34.5°/00 ) ...
... The hydrological stations established in spring (November 1972) along 70°E reveal at 46°S the northern limit of the 2°C isotherm and the presence of two fronts at 46 and 43°S, separated, from the surface to 300 rn, by · a relatively homogeneous water (temperature about 9°C, salinity about 34.5°/00 ) ...
Study Guide Questions – Earth Structure and Plate Tectonics What
... Broader application of radiometric dating revealed some really old (billions of years) pieces of continents, but the ocean basins were no older than about 200 million years The expanding field of paleomagnetics showed that the continents had moved independently of each other through time. And paleom ...
... Broader application of radiometric dating revealed some really old (billions of years) pieces of continents, but the ocean basins were no older than about 200 million years The expanding field of paleomagnetics showed that the continents had moved independently of each other through time. And paleom ...
Primary productivity
... • Sunlight strong enough to support photosynthesis occurs only to a depth of 100 meters (euphotic zone) Locations of maximum photosynthetic productivity • Margins of the oceans – Abundant supply of nutrients from land – Water shallow enough for light to penetrate all the way to the sea floor • Upwel ...
... • Sunlight strong enough to support photosynthesis occurs only to a depth of 100 meters (euphotic zone) Locations of maximum photosynthetic productivity • Margins of the oceans – Abundant supply of nutrients from land – Water shallow enough for light to penetrate all the way to the sea floor • Upwel ...
Earth Interior and Plate tectonics
... temperature 50oC(120oF) • Radioactive elements contribute to Earth's high internal temperature. Earth's interior contains radioactive isotopes (uranium, thorium and potassium- are quite rare), their nuclei break up, releasing energy as they become more stable. ...
... temperature 50oC(120oF) • Radioactive elements contribute to Earth's high internal temperature. Earth's interior contains radioactive isotopes (uranium, thorium and potassium- are quite rare), their nuclei break up, releasing energy as they become more stable. ...
What adaptations allow deep-sea creatures to survive in extreme
... Hydrothermal vents form where two continental plates collide. Cold seawater pours into the earth’s crust and encounters molten rocks. Water spewing back out of the vents’ chimneys might reach 700°F. A few feet away, water is barely above freezing. This unusual geology creates an extraordinary biolog ...
... Hydrothermal vents form where two continental plates collide. Cold seawater pours into the earth’s crust and encounters molten rocks. Water spewing back out of the vents’ chimneys might reach 700°F. A few feet away, water is barely above freezing. This unusual geology creates an extraordinary biolog ...
9.2 & 9.3 Plate Tectonics and Actions
... Ocean-Ocean Boundary: when 2 oceanic pieces converge, 1 goes under the other. Volcanoes form under the ocean. Ocean – Continental Boundary: when the continental plate converges with an oceanic plate, the less dense continental plate floats. May cause volcanic eruptions. Continental – Continent ...
... Ocean-Ocean Boundary: when 2 oceanic pieces converge, 1 goes under the other. Volcanoes form under the ocean. Ocean – Continental Boundary: when the continental plate converges with an oceanic plate, the less dense continental plate floats. May cause volcanic eruptions. Continental – Continent ...
plates
... What evidence do we have to support this idea? o Mid-ocean ridges are warmer than surrounding ocean floors o Active volcanoes on ridges, earthquakes on ridges o Mid-ocean ridge rocks are younger than surrounding ocean floor rocks o Mid-ocean ridge volcanoes are younger than volcanoes further away ...
... What evidence do we have to support this idea? o Mid-ocean ridges are warmer than surrounding ocean floors o Active volcanoes on ridges, earthquakes on ridges o Mid-ocean ridge rocks are younger than surrounding ocean floor rocks o Mid-ocean ridge volcanoes are younger than volcanoes further away ...
6.1_Notes_powerpoint
... crust where molten material, or magma comes to the surface. • Volcanic Activity is a constructive force that adds new rock to existing land or forms new islands. ...
... crust where molten material, or magma comes to the surface. • Volcanic Activity is a constructive force that adds new rock to existing land or forms new islands. ...
Chapter 4 Plate tectonics Review Game
... hardened lava are scattered across the ocean floor, this is evidence that molten material constantly erupts from the mid-ocean ridge ...
... hardened lava are scattered across the ocean floor, this is evidence that molten material constantly erupts from the mid-ocean ridge ...
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.