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5th Grade Science Curriculum Guide
5th Grade Science Curriculum Guide

... The student will investigate and understand how Earth’s surface is constantly changing. Key concepts include a) identification of rock types; b) the rock cycle and how transformations between rocks occur; c) Earth history and fossil evidence; d) the basic structure of Earth’s interior; e) changes in ...
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... The Mid-Atlantic Ridge is a divergent tectonic plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world. ...
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1. Oceans as a global challenge and priority

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... 10. The process occurring at the location labeled D is a. oceanic lithosphere being created. b. continental lithosphere being created. c. a continental-continental collision occurring. d. oceanic lithosphere being subducted. ...
Earth Geodynamic Hypotheses Updated
Earth Geodynamic Hypotheses Updated

... Philippine, Pacific, Antarctic, Cocos, and Nazca. Since that time this number has increased appreciably with the addition of many micro-plates. As we have seen, this hypothesis is based primarily on geophysical measurements; magnetic anomalies and earthquake seismology. Earth Expansion Hypothesis Ho ...
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Geological slant on plates

... from the core. The upper mantle is more brittle and is welded to the overlying crust. Together they form a layer called the lithosphere which is around 50km thick. Although the upper and lower mantle are effectively welded together, there is nevertheless a sharp division between the two called the M ...
Census of seafloor sediments in world`s ocean basins
Census of seafloor sediments in world`s ocean basins

... control the geologic accumulation of biogenic carbonate and silica as are very difficult to quantify, even on a local scale (e.g., 14, 15). Our digital map of seafloor sediments provides a missing link for constraining global relationships between the seafloor and the sea surface for which comprehe ...
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Ecosystems and the Physical Environment

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Meridional shifts of the Atlantic intertropical convergence zone since
Meridional shifts of the Atlantic intertropical convergence zone since

... the present (the past 25,000 years (25 kyr)) using data from an open-ocean transect of sediment cores. We compare these data to published continental and marine palaeohydrological records spanning 20◦ N to 15◦ S to develop a more comprehensive picture of ITCZ migrations. Sediment cores VM25-59, VM30 ...
Chapter 4 - Napa Valley College
Chapter 4 - Napa Valley College

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... secondary seismic waves begin to appear, this line indicates that the material is stiffer and less plastic (initiating the formation of magma), abounding silicates, oxides of magnesium and iron. The density of this area is about 4.6 tons/m3 and the temperature is 1400°K. From 1500 km (900 miles) to ...
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14332/16 - Europa.eu

... OCEANS AS A GLOBAL CHALLENGE AND PRIORITY ...
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Plate Tectonics The Two Types of Crust Physical Layers of the Earth

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CJK-2011-Report

... (nutrients, sulfur, iron, etc.) and biological properties (algae and zooplankton) of the Northwest Pacific ranging from open ocean to coastal regions (i.e. South and East China Seas, Yellow Sea). The presentations given by Hiroaki Saito, Daji Huang, Xinyu Guo and Jun Hu showed the importance of the ...
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Submarine hydrothermal vents: Hot springs on the seafloor OCN 201

... D probably none other anywhere ...
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tsunami - Pacific Disaster Net

... washing away entire villages. The inundation can also cause severe coastal erosion and affect areas upstream from the coast since tsunami waves can travel up rivers and streams from the ocean. ...
Lecture 5 - Academic Home Page
Lecture 5 - Academic Home Page

... On December 26, 2004 the most powerful earthquake in 40 years – and the third most powerful of the last century. Earthquakes around this region are quite common, the great difference with this earthquake is that it provoked the largest and deadliest tsunami in history. The quake began when part of ...
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EXECUTIVE SUMMARY Instrumentation for Arctic Ocean Exploration

... • wire and cable management within a dynamic ice pack • recovery of free-vehicles within ice-covered waters • under-ice navigation at high latitudes • remote monitoring of the water column and seafloor • maintaining an observational presence outside of the short (summer) Arctic field season. An impo ...
Key term
Key term

... A thin dense layer (6-10km thick), which lines the ocean floors. An older, thicker layer (usually 45 – 50km thick), which makes up the Earth’s landmasses. It is less dense than oceanic crust. Volcanoes can also form in the middle of plates, where plumes of hot magma rise upward and erupt onto the se ...
Interdisciplinary oceanographic observations
Interdisciplinary oceanographic observations

... the recognition of the challenging science embodied by the coastal oceans have drawn many oceanographers to coastal waters. Further, the ocean has been treated primarily as a continuum fluid for most physical oceanographic research, but particulates and dissolved matter (organic and inorganic) are o ...
Topic 12 Student Handout copy
Topic 12 Student Handout copy

... outer core. A section of the lithosphere that moves around Earth’s surface. A crack in a mass of rock or soil. The boundary between two plates spreading apart. A very fast, large ocean wave produced by an earthquake. The zone of Earth between the mantle and inner core. Thought to be liquid because e ...
Weather Presentation
Weather Presentation

... Drizzle is falling water droplets that have a diameter between 40 μm and 0.5 mm. Rain is falling water droplets that have a diameter between 0.5 mm and 5 mm. Sleet is ice pellets (frozen raindrops) that bounce upon impact with the ground. Snow is frozen water crystals that form below ...
Heat Transfer Tab
Heat Transfer Tab

... • What type of weather will occur after the High Pressure Cell comes through. • Describe the gradient (the increase/decrease or movement that characterizes what you are describing) that a High Pressure Cell moves to. Box 3: Low Pressure • What symbol is used to show Low pressure? • Describe the air ...
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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.
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