No Slide Title
... Seasonal Changes of the Winds The major wind belts both move and change with the seasons. The golden rule of seasonal wind changes is, Global wind systems follow the Sun. During July, when the Sun and the warmest air are north of the Equator, the ITCZ, the subtropical highs, and the subpolar lows a ...
... Seasonal Changes of the Winds The major wind belts both move and change with the seasons. The golden rule of seasonal wind changes is, Global wind systems follow the Sun. During July, when the Sun and the warmest air are north of the Equator, the ITCZ, the subtropical highs, and the subpolar lows a ...
Jeopardy
... A. Every year, oceans and lakes are bigger than the year before because of rain. B. Oceans and lakes will someday dry up because of evaporation. C. Oceans and lakes stay at about the same level because not enough water evaporates to affect water level. D. Oceans and lakes stay at about the same leve ...
... A. Every year, oceans and lakes are bigger than the year before because of rain. B. Oceans and lakes will someday dry up because of evaporation. C. Oceans and lakes stay at about the same level because not enough water evaporates to affect water level. D. Oceans and lakes stay at about the same leve ...
Cracking Up
... As the two sides of the rift valley pull even farther apart, the entire area will someday fall below sea level. Eventually, water from the Red Sea will rush in to fill the rift, spawning a new body of water. A million years from now— possibly sooner—the Great Rift Valley will lie at the bottom of an ...
... As the two sides of the rift valley pull even farther apart, the entire area will someday fall below sea level. Eventually, water from the Red Sea will rush in to fill the rift, spawning a new body of water. A million years from now— possibly sooner—the Great Rift Valley will lie at the bottom of an ...
CANT budgets in the ocean
... Figure 5. Uptake, storage, and transport of anthropogenic CO2 in the Atlantic Ocean (Pg C yr−1) based on (a) this study (weighted mean and standard deviation scaled to 1995), (b) the estimates of [Álvarez et al., 2003], where the transport across 24°N was taken from Rosón et al. [2003], (c) Wallace ...
... Figure 5. Uptake, storage, and transport of anthropogenic CO2 in the Atlantic Ocean (Pg C yr−1) based on (a) this study (weighted mean and standard deviation scaled to 1995), (b) the estimates of [Álvarez et al., 2003], where the transport across 24°N was taken from Rosón et al. [2003], (c) Wallace ...
What landforms are at different plate boundaries?
... • The difference between composite volcanoes which are associated with destructive plate margins and shield volcanoes which are associated with constructive plate margins. ...
... • The difference between composite volcanoes which are associated with destructive plate margins and shield volcanoes which are associated with constructive plate margins. ...
Key terms are bolded. 1.
... 107. What is the difference between point and nonpoint pollution? What are examples of each? Include sedimentation and stormwater runoff in your answer. o Point pollution is delivered directly into the water source. Nonpoint pollution reaches water source from runoff and erosion. Stormwater carries ...
... 107. What is the difference between point and nonpoint pollution? What are examples of each? Include sedimentation and stormwater runoff in your answer. o Point pollution is delivered directly into the water source. Nonpoint pollution reaches water source from runoff and erosion. Stormwater carries ...
Magnitude 8 Peru Earthquake of August 15, 2007
... at the Peru - Chile Trench and increase to > 300 km depth (blue dots) towards the east as the Nazca Plate dives deeper beneath the South American Plate. The epicenter of this M8.8 great earthquake is just 115 km (70 miles) NNE from Concepcion, an area of ~900,000 inhabitants that experienced severe ...
... at the Peru - Chile Trench and increase to > 300 km depth (blue dots) towards the east as the Nazca Plate dives deeper beneath the South American Plate. The epicenter of this M8.8 great earthquake is just 115 km (70 miles) NNE from Concepcion, an area of ~900,000 inhabitants that experienced severe ...
Where in the World was Lystrosaurus
... 8. Continental drift was not widely accepted when it was first proposed because ____. 1.Wegener couldn’t explain why or how the continents moved 2.continental landmasses were too big to move slowly over Earth’s surface 3.magnetic and sonar data proved that Wegener’s hypothesis was incorrect 4.mantle ...
... 8. Continental drift was not widely accepted when it was first proposed because ____. 1.Wegener couldn’t explain why or how the continents moved 2.continental landmasses were too big to move slowly over Earth’s surface 3.magnetic and sonar data proved that Wegener’s hypothesis was incorrect 4.mantle ...
Sediment Deposition Supports Seafloor Spreading
... during the lesson. To open the kmz file, open Google first and then select the File > Open menu. 3. The images are generally current to within the past three years. The Google Earth view of the ocean is digitally created so you can see the “look of the seafloor” without water. Of course, a real sat ...
... during the lesson. To open the kmz file, open Google first and then select the File > Open menu. 3. The images are generally current to within the past three years. The Google Earth view of the ocean is digitally created so you can see the “look of the seafloor” without water. Of course, a real sat ...
EARTH DIFFERENTIATES
... Atmosphere produces run-away greenhouse effect that raises Venus' surface temperature to over 450 deg C (hot enough to melt lead). Venus' surface hotter than Mercury's despite being nearly twice as far from the Sun. Venus probably once had lots of water like Earth that boiled away, leaving it quite ...
... Atmosphere produces run-away greenhouse effect that raises Venus' surface temperature to over 450 deg C (hot enough to melt lead). Venus' surface hotter than Mercury's despite being nearly twice as far from the Sun. Venus probably once had lots of water like Earth that boiled away, leaving it quite ...
oceanic ridges
... Mantle convection: Hotter mantle material rises beneath divergent boundaries, cooler material sinks at subduction zones. So: moving plates, EQs, & volcanic eruptions are due to Earth’s loss of internal heat. ...
... Mantle convection: Hotter mantle material rises beneath divergent boundaries, cooler material sinks at subduction zones. So: moving plates, EQs, & volcanic eruptions are due to Earth’s loss of internal heat. ...
thetheoryofplatetectonics
... What are the phases of the moon starting with the New Moon? Draw them. ...
... What are the phases of the moon starting with the New Moon? Draw them. ...
tsunamis - MrDanielASBSukMSSci
... the subduction zone where the India Plate dives under the Burma Plate. The seabed of the Burma plate is estimated to have risen several metres vertically up over the India plate, creating shock waves in the Indian Ocean that travelled at up to 800 km/h (500 mi/h), forming tsunamis when they reached ...
... the subduction zone where the India Plate dives under the Burma Plate. The seabed of the Burma plate is estimated to have risen several metres vertically up over the India plate, creating shock waves in the Indian Ocean that travelled at up to 800 km/h (500 mi/h), forming tsunamis when they reached ...
Chapter 14 The Ocean Floor
... The Atlantic Ocean is about half the size of the Pacific Ocean, and is not quite as deep. It is a relatively narrow ocean compared to the Pacific. The Atlantic and Pacific Oceans are bounded to the east and west by continents. The Indian Ocean is slightly smaller than the Atlantic Ocean, but it has ...
... The Atlantic Ocean is about half the size of the Pacific Ocean, and is not quite as deep. It is a relatively narrow ocean compared to the Pacific. The Atlantic and Pacific Oceans are bounded to the east and west by continents. The Indian Ocean is slightly smaller than the Atlantic Ocean, but it has ...
Kump_Ch07_TH - Camosun College
... • Thick fill or unconsolidated sediment amplifies ground motion due to surface waves: local geology & proximity both affect amplitude • More ground motion, more & infrastructure building damage ...
... • Thick fill or unconsolidated sediment amplifies ground motion due to surface waves: local geology & proximity both affect amplitude • More ground motion, more & infrastructure building damage ...
Abrupt Climate Change and Multistability of the Thermohaline
... cooled, and some of it changes phase. The North Atlantic experiences a net excess of evaporation over precipitation annually, and together with the formation of sea ice this increases the salinity. The resulting cold, salty water is denser than its surroundings, and it falls to a deeper level of the ...
... cooled, and some of it changes phase. The North Atlantic experiences a net excess of evaporation over precipitation annually, and together with the formation of sea ice this increases the salinity. The resulting cold, salty water is denser than its surroundings, and it falls to a deeper level of the ...
The Face of the Earth Continents and Oceans
... • Interactive Dynamic Processes at the Surface • Roles of the atmosphere (gases, winds, climate), ocean (rivers, waves, currents) and biology (cycles of growth and consumption) • Internal Dynamic Processes • Driven by the Earth’s radioactive heat • Energy release to the surface • Influences on Conti ...
... • Interactive Dynamic Processes at the Surface • Roles of the atmosphere (gases, winds, climate), ocean (rivers, waves, currents) and biology (cycles of growth and consumption) • Internal Dynamic Processes • Driven by the Earth’s radioactive heat • Energy release to the surface • Influences on Conti ...
Chemical Oceanography - 106Thursday130-430
... An organism's response to water temperature is considered to be cold blooded (or poikilothermic) or warm blooded (homeothermic) depending on their ability to control their internal body temperature. If any species is moved out of its temperature tolerance range it may die in a short time although t ...
... An organism's response to water temperature is considered to be cold blooded (or poikilothermic) or warm blooded (homeothermic) depending on their ability to control their internal body temperature. If any species is moved out of its temperature tolerance range it may die in a short time although t ...
Lesson 9: Karst, Coastal and Glacial features AM Celâl
... called Karren). In southern France, in the region of Languedoc, they are known as cairissa. The lapiaz form by the dissolution of the surface of the soluble rocks by the weak carbonic acid falling as rain. This dissolution can take the form of tiny rivulets or little pits or even pot-shaped small de ...
... called Karren). In southern France, in the region of Languedoc, they are known as cairissa. The lapiaz form by the dissolution of the surface of the soluble rocks by the weak carbonic acid falling as rain. This dissolution can take the form of tiny rivulets or little pits or even pot-shaped small de ...
Understanding the Cascadia Subduction Zone
... One way tectonic plates move is for an oceanic plate to sink underneath a continental plate as the two plates converge, called a subduction zone. Subduction zones create the largest earthquakes observed on the earth, such as the frequent earthquakes in Japan and Chile, so understanding these bounda ...
... One way tectonic plates move is for an oceanic plate to sink underneath a continental plate as the two plates converge, called a subduction zone. Subduction zones create the largest earthquakes observed on the earth, such as the frequent earthquakes in Japan and Chile, so understanding these bounda ...
Lab 2 Presentation slides
... a plastic region of earth's mantle called the asthenosphere. *Note that bottom figure is schematic and mantle lithosphere is much thicker than typical continental & oceanic crust. ...
... a plastic region of earth's mantle called the asthenosphere. *Note that bottom figure is schematic and mantle lithosphere is much thicker than typical continental & oceanic crust. ...
11 Sea Floor
... • Volcanoes outgasses water to fill oceans • Average depth = 4 km • Continental Margins mark edge of continent from deep sea floor – 2 types of margins ...
... • Volcanoes outgasses water to fill oceans • Average depth = 4 km • Continental Margins mark edge of continent from deep sea floor – 2 types of margins ...
Plate Tectonics and Weathering
... they have separated on the opposite side(s) When two plates separate lava or magma reaches the ...
... they have separated on the opposite side(s) When two plates separate lava or magma reaches the ...
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.