Unit 2 Terms
... forced up over the cooler, more dense air; Warm Moisture laden air cools at higher altitude; Cool air holds less moisture; Consequently clouds condense and rain falls. Convectional Rainfall - Usually occurs in hot areas like tropics or continental summer; Sun heats the earth causing large amounts of ...
... forced up over the cooler, more dense air; Warm Moisture laden air cools at higher altitude; Cool air holds less moisture; Consequently clouds condense and rain falls. Convectional Rainfall - Usually occurs in hot areas like tropics or continental summer; Sun heats the earth causing large amounts of ...
Climate - GeoInteractive
... 6. Pressure gradient is steep causing very fast winds which swirl around the centre. 7. Dry air at the top of the hurricane sinks into the calm ‘eye’ of the storm (the centre). 8. The winds and rain caused by hurricanes can kill many ...
... 6. Pressure gradient is steep causing very fast winds which swirl around the centre. 7. Dry air at the top of the hurricane sinks into the calm ‘eye’ of the storm (the centre). 8. The winds and rain caused by hurricanes can kill many ...
Ocean Food Chains - Santa Barbara Museum of Natural History
... Phytoplankton (plant plankton) and kelp are the main producers at the beginning of ocean food chains. These producers get their energy from the sun. Ocean animals, from sea stars to fish to marine mammals, depend on plankton for survival. Ocean animals are consumers. They can be catego ...
... Phytoplankton (plant plankton) and kelp are the main producers at the beginning of ocean food chains. These producers get their energy from the sun. Ocean animals, from sea stars to fish to marine mammals, depend on plankton for survival. Ocean animals are consumers. They can be catego ...
1 One of the most important aspects of understanding ocean life is
... particles passively intercepted by the spacecraft. Radar is an example of an active sensor. Data from the TOPEX/Poseidon satellite are used to map ocean currents whose patterns have a profound effect on ocean life. TOPEX/Poseidon actively generates radar pulses that bounce off the surface of the oce ...
... particles passively intercepted by the spacecraft. Radar is an example of an active sensor. Data from the TOPEX/Poseidon satellite are used to map ocean currents whose patterns have a profound effect on ocean life. TOPEX/Poseidon actively generates radar pulses that bounce off the surface of the oce ...
Volcanoes
... Made of lava and cinders Have steep peaks and sloping sides Mt. Fuji (Japan), St. Helens (USA) Mount Vesuvius in Italy Explode when they erupt ...
... Made of lava and cinders Have steep peaks and sloping sides Mt. Fuji (Japan), St. Helens (USA) Mount Vesuvius in Italy Explode when they erupt ...
Eastern United States
... • On the western side of the mountians the air rises and then descends on the eastern side. The air warms as it decreases in altitude creating warm currents and an effect called the “chinook winds.” This along with the low elevation and latitude creates higher temperatures in cities closer to the ea ...
... • On the western side of the mountians the air rises and then descends on the eastern side. The air warms as it decreases in altitude creating warm currents and an effect called the “chinook winds.” This along with the low elevation and latitude creates higher temperatures in cities closer to the ea ...
2nd 9 Weeks Test Review
... asthenosphere—taffy-like lower part of the mantle continental drift—plates have moved slowly to their current locations convergent boundary—plates move together; mountains form divergent boundary—plates move apart; volcanoes form transform boundary—earthquakes occur subduction zone—convergent bounda ...
... asthenosphere—taffy-like lower part of the mantle continental drift—plates have moved slowly to their current locations convergent boundary—plates move together; mountains form divergent boundary—plates move apart; volcanoes form transform boundary—earthquakes occur subduction zone—convergent bounda ...
Chapter 6 Study Guide
... a. The deflection is caused by the differential speed of rotation between Earth’s equator and polar regions, relative to an object moving across the Earth’s surface. b. Coriolis deflection increases poleward and as speed increases. C. Three major convection cells are present in each hemisphere. 1. T ...
... a. The deflection is caused by the differential speed of rotation between Earth’s equator and polar regions, relative to an object moving across the Earth’s surface. b. Coriolis deflection increases poleward and as speed increases. C. Three major convection cells are present in each hemisphere. 1. T ...
Read the article
... region (at times possibly caused by stronger than normal trade winds) and since there is an open communication across the Pacific Ocean this warm water has to flow eastward as an equatorial counter-current. In the mid 1970-ties the effect was thought to be localised to the South American coast and t ...
... region (at times possibly caused by stronger than normal trade winds) and since there is an open communication across the Pacific Ocean this warm water has to flow eastward as an equatorial counter-current. In the mid 1970-ties the effect was thought to be localised to the South American coast and t ...
Wegener—Continental Drift
... each other, forming volcanic cones. Continental crust sinking into the mantle and melting, coming back up as volcanoes. Oceanic crust subducting below continental crust, then melting and rising to the surface. Oceanic crust pushing against oceanic crust causing underwater volcanic peaks. ...
... each other, forming volcanic cones. Continental crust sinking into the mantle and melting, coming back up as volcanoes. Oceanic crust subducting below continental crust, then melting and rising to the surface. Oceanic crust pushing against oceanic crust causing underwater volcanic peaks. ...
Power Point Presentation
... Compression waves (Pwaves): travel by squeezing and expanding medium they travel through. They can travel through both solids and liquids (e.g., sound waves); Shear waves (S-waves): travel by shearing medium they pass through. S-waves can travel only through solids since particles need to be bonded ...
... Compression waves (Pwaves): travel by squeezing and expanding medium they travel through. They can travel through both solids and liquids (e.g., sound waves); Shear waves (S-waves): travel by shearing medium they pass through. S-waves can travel only through solids since particles need to be bonded ...
History of Plate Tectonics PPT
... • His hypothesis proposed that the continents had once been joined as a single landmass, called PANGAEA. • ‘Pangaea’ is a Greek word meaning ‘All the Earth’ ...
... • His hypothesis proposed that the continents had once been joined as a single landmass, called PANGAEA. • ‘Pangaea’ is a Greek word meaning ‘All the Earth’ ...
chapter 8
... then be used to calculate the velocity of the geostrophic flow, the volume of water transported and the depth of the flow. The central water of surface gyres is isolated in the interior of the gyres. An excellent example of this is the Sargasso Sea in the central North Atlantic where a lens of clear ...
... then be used to calculate the velocity of the geostrophic flow, the volume of water transported and the depth of the flow. The central water of surface gyres is isolated in the interior of the gyres. An excellent example of this is the Sargasso Sea in the central North Atlantic where a lens of clear ...
Smart Oceans Backgrounder
... and Internet connectivity to a broad suite of subsea instruments from the coast to the deep sea, supporting research on complex ocean and Earth processes in ways not previously possible. This Internet c ...
... and Internet connectivity to a broad suite of subsea instruments from the coast to the deep sea, supporting research on complex ocean and Earth processes in ways not previously possible. This Internet c ...
Chapter 16 Oceans, Shorelines and Shoreline Processes Exploring
... • Seasonal Changes in Beaches – Summer beaches usually have a wide berm, gently sloping beach face, and smooth offshore profile. – Winter beaches tend to be steeper and made up of coarser materials than summer beaches because waves are more energetic during this season. Berms may be absent. ...
... • Seasonal Changes in Beaches – Summer beaches usually have a wide berm, gently sloping beach face, and smooth offshore profile. – Winter beaches tend to be steeper and made up of coarser materials than summer beaches because waves are more energetic during this season. Berms may be absent. ...
Nutrient Cycles
... Coriolis Force affects ocean surface currents. The Coriolis Effect acts on moving water, because it is not attached to the rotating Earth. As water flows over the rotating earth, it appears to deflect to the right in the Northern Hemisphere and the left in the Southern. ...
... Coriolis Force affects ocean surface currents. The Coriolis Effect acts on moving water, because it is not attached to the rotating Earth. As water flows over the rotating earth, it appears to deflect to the right in the Northern Hemisphere and the left in the Southern. ...
The Dynamic Crust Topic 4 Topic 12 in Review Book
... A transform boundary occurs when two plates slide past one another. This dragging builds up potential energy which is eventually released as kinetic energy as earthquakes The San Andreas Fault is an example of this type of sliding boundary Convection Currents Convection currents drag or push plates ...
... A transform boundary occurs when two plates slide past one another. This dragging builds up potential energy which is eventually released as kinetic energy as earthquakes The San Andreas Fault is an example of this type of sliding boundary Convection Currents Convection currents drag or push plates ...
12earth6s
... core, solid mantle and crust Crust is broken up into plates which slide around on the upper mantle Plate tectonics and erosion constantly ...
... core, solid mantle and crust Crust is broken up into plates which slide around on the upper mantle Plate tectonics and erosion constantly ...
OCEAN BASINS, GEOGRAPHY AND GEOLOGY OF THE OCEANS
... EARTH – The earth is 4.5 billion years old and has inner defined regions. The floor is about 200my old and the continents are about 3.8 my old Inner core –1200km, 4000oC or 7200oF - solid Outer core – 1300km - liquid Mantle – 2850 km thick, semi-solid but flows Continental crust or lithosphere – 100 ...
... EARTH – The earth is 4.5 billion years old and has inner defined regions. The floor is about 200my old and the continents are about 3.8 my old Inner core –1200km, 4000oC or 7200oF - solid Outer core – 1300km - liquid Mantle – 2850 km thick, semi-solid but flows Continental crust or lithosphere – 100 ...
Seismic Waves Webquest - Dublin City Schools Dashboard
... 1. Go to http://aspire.cosmic-‐ray.org/Labs/SeismicWaves/ you can also access this website in the resources section of this lesson. 2. Spend 1-‐2 minutes playing with the Mighty Wave Make ...
... 1. Go to http://aspire.cosmic-‐ray.org/Labs/SeismicWaves/ you can also access this website in the resources section of this lesson. 2. Spend 1-‐2 minutes playing with the Mighty Wave Make ...
Paleomagnetism: Divergent Boundary
... destroyed at deep sea trenches. This was the missing link needed by Wegener to complete his model for continental drift. There are a dozen or so major plates and several smaller plates. Tectonic plates move in different directions and different rates over the Earth’s surface. Tectonic plates interac ...
... destroyed at deep sea trenches. This was the missing link needed by Wegener to complete his model for continental drift. There are a dozen or so major plates and several smaller plates. Tectonic plates move in different directions and different rates over the Earth’s surface. Tectonic plates interac ...
Part C 11. cyanobacteria 12. condensation 13. crust 14. sun 15. core
... cycle begins with the sun. Water evaporates from the earth’s surface, changing from a liquid into a gas. It then and rises into the atmosphere where it is cooled. Cooling causes water vapor to condense and forms clouds. When the clouds become saturated, the water returns to the Earth through precipi ...
... cycle begins with the sun. Water evaporates from the earth’s surface, changing from a liquid into a gas. It then and rises into the atmosphere where it is cooled. Cooling causes water vapor to condense and forms clouds. When the clouds become saturated, the water returns to the Earth through precipi ...
Word format
... What is the average depth of the ocean? __________________ Sunlight can only penetrate to a depth of about ______________ so the majority of the ocean is very dark and cold- only slightly warmer than freezing. The pressure in the ocean can reach as high as 1000 times atmospheric pressure. So we can ...
... What is the average depth of the ocean? __________________ Sunlight can only penetrate to a depth of about ______________ so the majority of the ocean is very dark and cold- only slightly warmer than freezing. The pressure in the ocean can reach as high as 1000 times atmospheric pressure. So we can ...
24. Ocean Basins p. 350-372
... What is the average depth of the ocean? __________________ Sunlight can only penetrate to a depth of about ______________ so the majority of the ocean is very dark and cold- only slightly warmer than freezing. The pressure in the ocean can reach as high as 1000 times atmospheric pressure. So we can ...
... What is the average depth of the ocean? __________________ Sunlight can only penetrate to a depth of about ______________ so the majority of the ocean is very dark and cold- only slightly warmer than freezing. The pressure in the ocean can reach as high as 1000 times atmospheric pressure. So we can ...
Physical oceanography
Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.