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A unifying view of climate change in the Sahel linking intra
A unifying view of climate change in the Sahel linking intra

... blue is early red is late ...
The Earth
The Earth

... sea floor and measuring their distance from the ridge crest. • Continents are moved by the expanding sea floor - they ride on larger blocks we call “Lithospheric Plates”. ...
Plate Tectonics
Plate Tectonics

... Plates move against each other Stress builds up ...
Plate Tectonics Study Guide: Answer key
Plate Tectonics Study Guide: Answer key

... Land forms to know ➢ Mountains: created when continental crust converge with other crust. No volcanoes when 2 continental crust come together ➢ Coastal mountains: Mountains near coast, associated with Oceanic Continental convergent boundary These mountains will have volcanoes ...
Composition of the earth, Geologic Time, and Plate Tectonics
Composition of the earth, Geologic Time, and Plate Tectonics

... pob = pl + p f pob: Overburden pressure pl : Lithostatic pressure pf : Fluid pressure ...
PLATE TECTONICS
PLATE TECTONICS

... People Didn’t Get Wegener’s “Drift” … - So, without an explanation for how these plates were moving, people didn’t believe Wegener’s theory. They needed more proof for how huge continents could “drift.” - Then World War II came, and with it, technology. After WWII, oceanographers began to use more ...
Giant Lava Flows, Mass - Lamont
Giant Lava Flows, Mass - Lamont

... large area. Structural data from rift basins in the southeastern United States suggest that they ceased subsidence and underwent tectonic inversion (under compression in the same direction in which they were previously under extension) close to the focus of the CAMP before or at the time of its empl ...
Plate Tectonics PowerPoint
Plate Tectonics PowerPoint

... • When two oceanic plates collide, one runs over the other causing it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a deep-sea trench. • The deepest parts of the ocean are found along trenches. – Th ...
Terra Nova 2012 Jagoutz
Terra Nova 2012 Jagoutz

... tonalite-trondhjemite-granodiorite (TTG) upper continental crustal rocks in Archean times, compared to dominant potassiumenriched granite-granodiorite (GG) associations in the post-Archean upper continental crust. The transition between TTG and GG dominated upper crust occurred approximately around ...
Australasian Regional IODP Workshop in 2017 for building new
Australasian Regional IODP Workshop in 2017 for building new

... platforms. The proposed workshop will identify the leading scientific ideas, hypotheses and questions for this region that are pressing and require ocean drilling. The region's extensive plateaus and basins can provide crucial sedimentary records to help understand the developing interactions betwe ...
Geology of the Hawaiian Islands
Geology of the Hawaiian Islands

... Main mechanism of chemical weathering that removes atmospheric CO2 Reaction of silicate minerals with carbonic acid to form clay minerals and dissolved ions Summarized by the Urey reaction ...
HiQ VERISEQ Carbon dioxide
HiQ VERISEQ Carbon dioxide

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Powerpoint

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Volcanoes: lecture 1

... Increase temperature with depth Varies depending on tectonic setting Average increase is 25 degrees C/KM Yellow dotted line indicates 500 degrees centigrade ...
Geology of Oceanography
Geology of Oceanography

... carbonate more soluble in seawater – It also more soluble in the lower temperature of the deep water – At a certain point, calcium carbonate dissolves as fast as it forms= carbonate compensation depth ...
Layers of Earth Notes - Laveen Teacher Sites
Layers of Earth Notes - Laveen Teacher Sites

...  *Mostly made up of magma (molten rock)  *Has convection currents which cause the crust to move  *Average temperature is about 3000°C ...
ENVI 21 Life in the Ocean
ENVI 21 Life in the Ocean

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VERISEQ® pharmaceutical grade gases. Carbon→dioxide.
VERISEQ® pharmaceutical grade gases. Carbon→dioxide.

... →→ Product sheet, Speciality gases ...
Lecture 2b: Hot spots
Lecture 2b: Hot spots

... – Then heat flow, a slow process, raises the temperature of the cold nonconvecting part of the mantle attached to the base of the continent until it melts over a wide area, in a process that is characterized by positive feedback between melting and heat flow, giving high magma flux for a short time. ...
Pachamama Geography Consultants
Pachamama Geography Consultants

... from MT. Rainer National Park. Sections of the town are composed of solidified mud flows that originated on Mt.Ranier. ...
Plate Boundary Notes
Plate Boundary Notes

... Evidence of Continental Drift ...
Sulfate Reducing Bacteria (SRB) Dr. Richard Cresswell Practice
Sulfate Reducing Bacteria (SRB) Dr. Richard Cresswell Practice

... organisms can also be beneficial by removing sulfate and heavy metals from waste streams and are commonly used in the coal and metal mine industry to remediate leachate from acidwaste tailings and abandoned mines Where do you find SRBs? SRB are ubiquitous and can be found in many natural and enginee ...
pdf - University of Colorado Boulder
pdf - University of Colorado Boulder

The Caribbean – overlooked hydrocarbon potential on N America`s
The Caribbean – overlooked hydrocarbon potential on N America`s

... seamounts push up through overlying upper Cretaceous – Recent sediments are very similar in appearance to Sigsbee salt knolls of the Gulf of Mexico. At least some are salt diapers, with indications of adjacent rim synclines, Other parts of the Caribbean Plate, west and southeast of the plateau, rese ...
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 ...
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Anoxic event



Oceanic anoxic events or anoxic events (Anoxia conditions) refer to intervals in the Earth's past where portions of oceans become depleted in oxygen (O2) at depths over a large geographic area. During some of these events, euxinia develops - euxinia refers to anoxic waters that contain H2S hydrogen sulfide. Although anoxic events have not happened for millions of years, the geological record shows that they happened many times in the past. Anoxic events coincide with several mass extinctions and may contribute to these events. These mass extinctions include some that geobiologists use as time markers in biostratigraphic dating. It is believed oceanic anoxic events are strongly linked to slowing of ocean circulation, climatic warming and elevated levels of greenhouse gases. Enhanced volcanism (through the release of CO2 and other greenhouse gases) is the proposed central external trigger for the development of these events.
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