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MONTE ARCI GEOMUSEUM Stefano Incani Masullas Museum
MONTE ARCI GEOMUSEUM Stefano Incani Masullas Museum

... written by V. Angius and G. Casalin around mid-nineteenth century. ...
ESEarthquakes - Cole Camp R-1
ESEarthquakes - Cole Camp R-1

... ✦S waves cannot be detected on the opposite side of the earth from the earthquake's epicenter. ...
Plate Tec Review Sheet 2016 Answers
Plate Tec Review Sheet 2016 Answers

... SUBDUCTION OCCURS AT CONVERGENT BOUNDARIES CREATING TRENCHES AND VOLCANOES 4. Draw a picture and describe a transform boundary. SHOULD DRAW A PICTURE OF TWO BOXES WITH ONE ARROW POINTING UP AND ONE POINTING DOWN; AT TRANSFORM BOUNDARIES THE PLATES SLIDE PAST EACH OTHER OR MOVE PAST EACH OTHER IN OPP ...
Oceanography—Plate Tectonics Name
Oceanography—Plate Tectonics Name

... the various plates around. Notice particularly where on Earth each type of interaction can be found. (Look at the little map!) This simulation models the four types of plate interactions that occur on Earth. 6. What are the four different types of boundaries between tectonic plates? ...
IDS 102 Plate Tectonics Questions Part I: Observations
IDS 102 Plate Tectonics Questions Part I: Observations

... 7. Explain how basaltic magmas are formed in the upper mantle. At plate margins that are diverging, the asthenosphere rises into the region where the plates separate. If the rock in the asthenosphere moves toward the Earth’s surface, the lithostatic pressure will decrease. This change in pressure ca ...
Energy from Earth`s interior supports life in global ecosystem
Energy from Earth`s interior supports life in global ecosystem

... from the ones that support life in both the mud layers in the sea bed and the oceanic water column. It is possible that life based on chemosynthesis is found on other planets, where Active life or dead relics? the chemical environment permits. Our continued Dr Lever's basalt is 3.5 million years old ...
Chapter 14 The Ocean Floor
Chapter 14 The Ocean Floor

...  Nearly 71% of Earth’s surface is covered by the global ocean  The oceans haven’t really been a huge focus of study until the late 1800’s  As technology becomes better, it allows us to study what happens underneath the oceans  Oceanography  a science that draws on the methods and knowledge of g ...
Mineral resource
Mineral resource

... Figure 15-19 ...
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The Caribbean – overlooked hydrocarbon potential on N America`s

Convergent Plate Boundary Diagrams
Convergent Plate Boundary Diagrams

... 3._________________________________________ 6. _________________________________________ a. What is created during a continental-continental collision? ...
IGCSE Revision document
IGCSE Revision document

... If a metal is more reactive than hydrogen its ions stay in solution and hydrogen bubbles off ...
Sea Floor Spreading LAB 2017
Sea Floor Spreading LAB 2017

... continually been forming over millions of years at the mid-ocean ridges. Hess found that on each side of the ridge, sea floor got older as a person moved away from the ridge towards the continents. The older, denser oceanic crust eventually descends into deep trenches along the continents and is rec ...
NOAA Mid Oceanic Ridges
NOAA Mid Oceanic Ridges

... 11. Along the rift valley, divergence leads to volcanism that creates new oceanic crust, crust that is in its turn _______ and _____________ by continued divergence and volcanism. 12. By this perpetual process, oceans -_____ and _______slowly but surely. An example occurs at the Juan de Fuca Ridge, ...
Changes to Earth`s Surface
Changes to Earth`s Surface

... were to heat up, it would explode. ...
Fact Sheet - SharpSchool
Fact Sheet - SharpSchool

... based on several assumptions about the tectonic process. First, the new material is producing by sea-floor spreading at the mid-ocean ridges, which once formed become part of a plate, second the surface area is protected, therefore plate material must be destroyed through another process, and last o ...
Earthsci1
Earthsci1

... mantle, largely composed of oxygen, magnesium and silicon in the ratio of 4:2:1, further divided into two shells, an inner shell called the asthenosphere, and an outer shell called the lithosphere; an outer crust composed of two components, one represented by the sea floors and the other by the cont ...
From Plate Tectonics to Climate
From Plate Tectonics to Climate

Oceanography – EXAM 1 Review Questions
Oceanography – EXAM 1 Review Questions

Earth’s Layers
Earth’s Layers

... Summarize the 3 layers of Earth on the basis of relative position , density and composition. ...
Growing or
Growing or

... significance to continental crust and hydrosphere, water and potassium. New basaltic ocean floor forms at a rate of about 10 km3 yr-' and most must be subducted The subducted ocean floor crust becomes hydrated before subduction (chlorite,epidote. serpentine, etc.) and most spilites have aboul five p ...
First stop – the CRUST
First stop – the CRUST

... third of Earth’s mass, but only about 15 % of its volume. ...
Lecture 12
Lecture 12

... Why the Redfield Ratios?? From a chemistry point-of-view. Each class of organic compounds has its own unique stoichiometry carbohydrates are C rich but N and P poor (e.g. (CH2O)n) proteins are C and N rich but P poor (e.g. amino acids) nucleotides are rich in both N and P (e.g. 4 bases) lipids are ...
earth`s components & characteristics
earth`s components & characteristics

... – Outer core- 3480 km thick, liquid iron, creates magnetic field ...
Earth`s Layers PowerPoint
Earth`s Layers PowerPoint

... How do we know there are layers of the earth? •Earthquakes emit different kinds of seismic waves that can travel through different substances and at different speeds •Scientists used these waves to determine the layers based on the speed and movement of the layers! ...
Earth
Earth

... fluid = liquid iron. 2. Liquid iron must circulate so rapidly in the Outer Core. 3. Earth must have a fast rotation: makes one revolution (spin) on its axis every 24 hours. ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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