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Jupiter and Its Moons Jupiter`s Atmosphere
Jupiter and Its Moons Jupiter`s Atmosphere

... • Smaller than the Moon, about 20% the size of the Earth ...
Geology of the Yorkshire Dales National Park
Geology of the Yorkshire Dales National Park

... Gorges and classic V-shaped valleys have been cut into the landscape by glacial melt water. It is thought that the gorges were cut through frozen rock during glacial and immediately post glacial times. This accounts for their narrowness and sheer sides. In many cases these are now dry valleys, the s ...
Running Water
Running Water

...  Lots of water, but hard to collect because of how it attaches to rocks and soil Zone of Saturation  Below top of water table ...
- bYTEBoss
- bYTEBoss

... Let’s see what it is really like! Antarctica’s ice sheet is constantly on the move. Huge rivers of ice known as glaciers are pulled slowly by gravity from the interior towards the sea. Along the way, the ice cracks, breaks and is ruptured by underlying rock. Crevasses up to hundreds of metres deep ...
Chapter One – Fire and Ice
Chapter One – Fire and Ice

... badly damaged or destroyed. Officials estimate that ...
Environmental Problems
Environmental Problems

... • The 8 warmest years have occurred since 1998 • Earth’s surface temperature has risen 0.8°C (1.4°F) in last 140 years. ...
The Illustrated History of GLACIAL EROSION
The Illustrated History of GLACIAL EROSION

... Sometimes the glacial till is deposited in mounds or hills. These are called DRUMLINS. The drumlins above are found in Scotland but similar features are found all over the northern hemisphere. Often drumlins are so large that they cannot be appreciated for what they are except when photographed fro ...
Quaternary Climate Change and Geomorphology
Quaternary Climate Change and Geomorphology

... Earth orbital parameters suggest that changes in the orbit of the Earth about the Sun may cause climate change from glacial to interglacial. ...
Oil Spill Detection and Tracking Technologies
Oil Spill Detection and Tracking Technologies

... • In GoM, Louisiana had no HF radars, offer to do emergency install got bogged down in government inter-agency discussions, never happened: could have improved shore party deployments • Off Alaska North Slope and Canada coastal coverage is incomplete, but new remote power developments could facilita ...
RM115
RM115

... rocky shore further south. To the north of the tidal mud flat there is an old bulkhead, with another tidal flat to the north of the bulkhead, rip rap in sections. The banks have been altered at the bulkhead (entire ice house area is likely dredge spoil), wood and debris are collected in the southern ...
- NERC Open Research Archive
- NERC Open Research Archive

... One Sentence Summary: Retreat of the Larsen Ice Shelf grounding line was complete 12 ka indicating recent disintegration was associated with surface climate, not oceanographic forced instability. ...
Document
Document

... Tide gauge shows land rising today ...
glacier_presentation_2004
glacier_presentation_2004

... When continental glaciers move across the landscape they pick up a lot of material and move forward. This is called advancing. When the glacier stops moving forward, they will melt, this is called retreating. ...
Weathering and Erosion
Weathering and Erosion

... visualization ...
Weathering and Erosion Powerpoint
Weathering and Erosion Powerpoint

... visualization ...
Weathering and Erosion
Weathering and Erosion

... visualization ...
Isostasy and Large Scale Gravity Chap. 9 Homework Answers (Dec
Isostasy and Large Scale Gravity Chap. 9 Homework Answers (Dec

... like a liquid) due the application of loads (e.g., ice sheets, erosion) over millions of years AND transmit earthquake induced shear waves with wave periods of <100 s. The logic goes, if the earth behaves as a ‘liquid’ to long time scale load, and hence is ‘like a liquid’ internally, then since (ide ...
Relaxation time
Relaxation time

... Glacial isostasy ...
An Introduction to the Geology and Fossils of Essex
An Introduction to the Geology and Fossils of Essex

... The environment of the region was now to change dramatically leading to the deposition of the London Clay, a mud laid down on the floor of a subtropical sea some 50 million years ago. The London Clay has yielded fine fossils of the sea's inhabitants such as molluscs, lobsters, crabs and sharks. Ther ...
7th Grade Science Unit 3 Vocabulary Uniformitarianism
7th Grade Science Unit 3 Vocabulary Uniformitarianism

... the past can be explained by current geologic processes. ...
The role of volcano-ice interactions in understanding
The role of volcano-ice interactions in understanding

... The vast majority of the glacierized volcanoes on Earth are in subduction zones (Fig. 1 from Edwards and Kochtitzky 2015; Iceland and Antarctica are the two notable exceptions), yet little work has been done in that setting to understand how interactions between ice loading and unloading may have ...
glagierSlides
glagierSlides

... Differences between Glacier & River Valleys ...
Physical Geography: Landforms
Physical Geography: Landforms

... Oxidation – oxygen combines with iron which decomposes rock Hydrolysis – chemical reaction when water and minerals interact Carbonation – carbon dioxide in the atmosphere dissolves in water, creating acid, which decomposes the rock. ...
chapter 17 - Geoclassroom Home
chapter 17 - Geoclassroom Home

... bring about climatic changes that produce glacial-interglacial intervals. Figure 17.18 According to the Milankovitch Theory, Minor Irregularities in Earth’s Rotation and Orbit May Affect Climatic Changes 11. The causes of short-term climatic changes such as occurred during the Little Ice Age are unk ...
Insolation Control of Ice Sheets
Insolation Control of Ice Sheets

... bedrock 1.0 km. – This would lower the ice sheet’s surface elevation 1.0 km • Resulting 6.5o C change in temperature • Large effects on mass balance of the ice sheet. ...
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Cryosphere



The cryosphere (from the Greek κρύος kryos, ""cold"", ""frost"" or ""ice"" and σφαῖρα sphaira, ""globe, ball"") is those portions of Earth's surface where water is in solid form, including sea ice, lake ice, river ice, snow cover, glaciers, ice caps, ice sheets, and frozen ground (which includes permafrost). Thus, there is a wide overlap with the hydrosphere. The cryosphere is an integral part of the global climate system with important linkages and feedbacks generated through its influence on surface energy and moisture fluxes, clouds, precipitation, hydrology, atmospheric and oceanic circulation. Through these feedback processes, the cryosphere plays a significant role in the global climate and in climate model response to global changes. The term deglaciation describes the retreat of cryospheric features.
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