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Chapter three worksheet 2012-13
Chapter three worksheet 2012-13

... a. Surface waters of the ocean are warmed by the _________________________ i. The surface waters can be as deep as _________________m b. The sun does not reach the ____________________ which are much colder at ___C. 35. The ______________________ is a zone if rapidly changing temperatures. a. The th ...
Earth Processes vocab and notes
Earth Processes vocab and notes

... 1. Landform: a physical feature on Earth’s surface 2. Weathering: the process of breaking rock into soil, sand, and other tiny pieces (sediment) 3. Erosion: the process of moving sediment from one place to another 4. Deposition: the process of dropping, or depositing, sediment in a new location 5. P ...
1What Makes Up the Earth?
1What Makes Up the Earth?

... Landforms are on the surface of the earth. The picture shows what the inside of the earth looks like. Notice that the earth is made up of layers. How many layers do you see? The top layer is the crust. It is 8 to 65 kilometers thick. The crust is made of rocks and soil. Mountains, plains and plateau ...
volcanoes - Etiwanda E
volcanoes - Etiwanda E

... • Effects of Plate Tectonics • Forces from Within the Earth ...
86:12 And by the Earth full of cracks/faults
86:12 And by the Earth full of cracks/faults

... Geologists said Tuesday the crack was a joint in the earth's crust. They believe the opening is the result of a weak point in the joint where one spot slips away from the other. Some parts measure more than 30feet deep and it drained what used to be a pond. Experts say earth cracks are common but th ...
Earth Layers and Continental Drift
Earth Layers and Continental Drift

... (includes liquids and gases); Heat transfer is caused by differences in temperature and density within a fluid (Ex: Water on a stove – water heats at the bottom of the pan, becomes less dense and rises; away from the heat source the water cools, becomes more dense and sinks; the process begins again ...
Global Surveyor finds stripes on Mars
Global Surveyor finds stripes on Mars

... flotilla of satellites were able to pin down events in the first 100 milliseconds of radiation received, establishing, among other things that a crack around 5 kilometres across formed on the neutron star, writes Peter Bond. On 27 December 2004 the radiation from an extremely powerful explosion on t ...
ppt: EarthInteriorJeopardy20Q
ppt: EarthInteriorJeopardy20Q

... B. Yes, when the magnetic field reverses. ...
plate tectonics study guide
plate tectonics study guide

... They receive more direct sunlight all year long than the poles do. 3. What causes tides? The gravitational pull of the moon as it revolves around the Earth. 4. What would happen if the gravity between the Sun and Mars increased? The Suns gravity would pull Mars closer and closer to it, eventually co ...
Earthquakes - TeacherWeb
Earthquakes - TeacherWeb

... Warm up What is an earthquake? What causes them? Where do they occur? ...
Maps and Map Projections
Maps and Map Projections

... A. Properties of the earth 1. sphere 2. rotates on polar axis (N/S poles)  day/night 3. polar axis tilted at 23.5 B. Locating places on the earth – creating a grid system 1. latitude/longitude 2. cardinal directions: N, S, E, W 3. 3 fixed points: a. center of earth b. north pole c. south pole 4. g ...
Module E: Unit 4, Lesson 1 – Earth`s Layers
Module E: Unit 4, Lesson 1 – Earth`s Layers

... • Oceanic crust is denser than continental crust because it contains almost twice as much iron, calcium, and magnesium. • The mantle is located between the crust and the core. • The mantle is a region of hot, slow-flowing solid rock. • The mantle contains more magnesium and less aluminum and silicon ...
Chapter 7 Earth and the Terrestrial Worlds
Chapter 7 Earth and the Terrestrial Worlds

... Internal Heat Drives Geological Activity Convection:  hot rock rises,  cool rock falls  (because hot rock is  less dense, just like  hot air is less dense) 1 convection cycle on  Earth takes about  100 million years ...
WORLD GEOGRAPHY:
WORLD GEOGRAPHY:

... ■ 1800 miles thick ■ solid but upper levels may be pliable ➢ Crust - rocky surface layer and thin ■ 5 miles thick below oceans ■ 22 miles thick below continents (uneven) ...
Physical Science - Blue Valley Schools
Physical Science - Blue Valley Schools

... The balloon was attracted to the wall because the balloon and the wall both carried the same ...
Science Ch 5 webnotes
Science Ch 5 webnotes

... Seismometer: instrument that detects and measures waves produced by earthquakes Primary (P) waves: fastest; pass through solid and liquid layers; move back and forth Secondary(S) waves: half as fast; only through solid layers; move up and down Surface (L) waves: slowest like ripples on a pond; on Ea ...
Chapter 20
Chapter 20

... each other, plates can be pushed upward and downward, Where plates move away from each other, molten forming mountain ranges, lava can rise up from below, some with volcanic activity, causing volcanic activity earthquakes ...
Chapter 1
Chapter 1

... • Earth forms (mountains, Grand Canyon, rock layers, fossils found high in the mountains) were due to catastrophic forces that shaped the world in a relatively short time. • Leads to ‘Young Earth’ concept • Bishop James Ussher of Ireland ...
Chapter 4 Babbey
Chapter 4 Babbey

... • A convection current is the flow that transfers heat within a fluid. • These change when temperature, density, or gravity act on the fluid. ...
Models of the Earth Section 1 Finding Direction
Models of the Earth Section 1 Finding Direction

... Latitude, continued Degrees of Latitude • Latitude is measured in degrees, and the equator is 0° latitude. The latitude of both the North Pole and the South Pole is 90°. • In actual distance, 1° latitude equals about 111 km. Minutes and Seconds • Each degree of latitude consists of 60 equal parts, c ...
03 Natural Causes of Climate Change
03 Natural Causes of Climate Change

... stratosphere over the year following the eruption. The total mass of SO2 of about 17 million tons being ejected. This very large stratospheric injection resulted in a reduction in the normal amount of sunlight reaching the Earth's surface by roughly 10%. This led to a decrease in northern hemisphere ...
The Five Themes of Geography
The Five Themes of Geography

... distances to cross: linear, time, and psychological. Linear refers to how far something must travel. It is affected by physical features on the earth. ...
International Year of Planet Earth – Activities and Plans in Mexico
International Year of Planet Earth – Activities and Plans in Mexico

... Mineral and Energy Resources and Life (Biodiversity in Mexico). In 2008, special events are planned on the Megacities program. The metropolitan area of Mexico City, with around 20-24 million inhabitants presents special challenges, being at high altitude within an active tectonic and volcanic area r ...
Document
Document

... • If one plate is capped by oceanic crust and the other by continental crust, the less dense, more buoyant continental plate will override the denser, oceanic plate. The oceanic plate sinks along what is known as a subduction zone, a zone where an oceanic plate descends into the mantle beneath an ov ...
How The Earth Works
How The Earth Works

... 35 minutes to birth of Christ 1 hour+ to pyramids 3 hours to retreat of glaciers from Wisconsin 12 days = 1 million years 2 years to extinction of dinosaurs 14 years to age of Niagara Escarpment 31 years = 1 billion years ...
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Spherical Earth



The concept of a spherical Earth dates back to around the 6th century BC, when it was mentioned in ancient Greek philosophy, but remained a matter of philosophical speculation until the 3rd century BC, when Hellenistic astronomy established the spherical shape of the earth as a physical given. The paradigm was gradually adopted throughout the Old World during Late Antiquity and the Middle Ages. A practical demonstration of Earth's sphericity was achieved by Ferdinand Magellan and Juan Sebastián Elcano's expedition's circumnavigation (1519−1522).The concept of a spherical Earth displaced earlier beliefs in a flat Earth: In early Mesopotamian mythology, the world was portrayed as a flat disk floating in the ocean and surrounded by a spherical sky, and this forms the premise for early world maps like those of Anaximander and Hecataeus of Miletus. Other speculations on the shape of Earth include a seven-layered ziggurat or cosmic mountain, alluded to in the Avesta and ancient Persian writings (see seven climes).The realization that the figure of the Earth is more accurately described as an ellipsoid dates to the 18th century (Maupertuis).In the early 19th century, the flattening of the earth ellipsoid was determined to be of the order of 1/300 (Delambre, Everest). The modern value as determined by the US DoD World Geodetic System since the 1960s is close to 1/298.25.
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