Dry Valleys, Antarctica 77°00' S Latitude 162°52' E Longitude (31 December 2004 – 3 February 2005)

Slides:



Advertisements
Similar presentations
Glaciers, Desert, and Wind
Advertisements

Glaciers, Desert, and Wind
How Glaciers Move ___________________ ____________ ______ __________
Glaciers Chapter 15.1.
This valley glacier has bands that look like ripples
Chapter 17 Review.
. Antarctica is a large continent located at the far south of the world. It is larger than Europe. The weather there is very cold. About 98% of Antarctica.
Dirty Ice or Icy Dirt?. Soil Moisture Saturation UNDER-SATURATED Not enough water to fill all of the pore space of a given soil SATURATED Just the right.
Glacial Processes and Landforms. What is a glacier? How do glaciers form?
Glacial Geomorphology Lab 10. Concepts Glacier Formation Accumulation and Ablation, Sublimation Movement Glacial Mass Balance Categories of Glaciers Where.
Erosion and Deposition by Glaciers Created By: Belinda Schmahl.
Charity I. Mulig.
How many kilometres from Ireland?? Antarctica is the world’s last great wilderness. It is a continent almost entirely buried by snow and ice. It is so.
7.1 Glaciers.
Chapter 7: Erosion and Deposition
Formation  Snow accumulation  More winter snowfall than summer melt  Glacier formation is similar to sedimentary rock formation.
How do Glaciers affect the land? WED V17. What is a glacier? 0 A large, long-lasting mass of ice which forms on land and moves downslope because of gravity.
Ch. 15 Glaciers.
Erosion and Deposition
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
Erosion An Examination of the Erosional Agents That Shape Our Land.
Glaciers Galore Ice Queen Period 1 Earth Science Honors November 30, 2013 The last Ice Age (Wisconsian) occurred over the last 2-3 million years (1). The.
Glaciation. "What causes ice sheets to expand and contract? Are the present ice sheets growing or shrinking? How will global warming impact the ice sheets?
Chapter 8.
Chapter 5: Section 2 Surface Processes and Landscapes
Chapter 7.1 Glaciers.
WHAT DO YOU ALREADY KNOW ABOUT THEM ? ANSWER TRUE OR FALSE.
Glacial Processes and Landforms What is a glacier? How do glaciers form?
Charity I. Mulig.
Glaciers.
Earth Science: 7.1A Glaciers. Glaciers  As recently as 15,000 years ago, up to 30 percent of earth’s land was covered by an glacial ice.  Earth was.
Section 15.1 What is a glacier?. Compare a River to a Glacier Fast flow Liquid: rain or snow
Glaciers Moving Ice Formation of Glaciers A glacier is defined as a mass of moving ice. A glacier is defined as a mass of moving ice. There are several.
Sea Ice, Ice Shelves, and Polynyas. Sea Ice Formation --in Antarctica, begins forming in late summer with winds from the continent, evaporative cooling.
SIHC - Glaciation. Glaciation Erosion by bodies of moving ice.
Changing Earth’s Surface Changing Earth's Surface Weathering –The process that breaks down and changes rocks that are exposed at Earth’s surface 8.1.
Glacial Erosion.
Glaciers Galore Ice Queen Period 1 Earth Science Honors November 30, 2013 The last Ice Age (Wisconsian) occurred over the last 2-3 million years (1). The.
Glaciers and Erosion Chapter 7 Section 1.
GLACIERS A glacier is: Any large mass of ice that moves slowly over land Any large mass of ice that moves slowly over land.
Glaciers. What is a glacier?  Glacier- A large moving mass of snow and ice.
Guided Notes For Glaciers Section 8.3. Glaciers shape the landscape by eroding, transporting, and depositing huge volumes of rock and sediment.
Changing Earth’s Surface
By Daniel and Faniza ANTARCTICA.. Antarctica is the fifth largest continent. Its land is covered by a huge ice cap without its ice cap, Antarctica would.
Glaciers & Erosion. Glaciers: What are they? very powerful agent of erosion mass of moving ice How are glaciers formed? when snow and ice accumulate to.
McMurdo Dry Valleys: safety protocols in a changing landscape.
Oxygen stable isotopes and chloride concentration in the surface waters of Taylor Valley Lakes, Antarctica, during the past 40 years Julie M. Brown*, W.
Glaciers.
Masses of Ice that: 1)Are at least 100 m thick 2)Originate on land 3)Move How Glaciers Form.
Ice is Ice---isn’t it? Why are glaciers and ice sheets important? Large volume of fresh water is stored in ice masses Change in ice volume affects global.
© Copyright University of Waikato. All rights reserved. | Contexts > Icy Ecosystems > Researching.
Glacial Processes and Landforms
GLACIERS Any large mass of ice that moves slowly over land.
Glaciers Chapter 3 Section 4. Standards  S 6.2a Surface water flow, glaciers, wind, and ocean waves have all been and continue to be active throughout.
Glaciers Chapter 3 Section 4 Pages Objective: Describe the causes and types of glaciers, how they impact land features, and analyze their role.
Chapter 3 Erosion and Deposition Section 4 Glaciers
CGC 1D1 Mr. Zapfe.  Final changes occurred which gave Canada’s landforms their present shape  Continuing collision of North American and Pacific Plates.
Glaciers Chapter 3 Section 4 Standards S 6.2a Surface water flow, glaciers, wind, and ocean waves have all been and continue to be active throughout.
UNIT 5WEATHERING: (B) GLACIERS Glacier-large long-lasting mass of snow compacted & recrystallized, first into firn then glacial ice. Glaciers part of hydrosphere.
Chapter 7.3 Glaciers. Glacier Any large mass of ice that moves slowly over land. Two kinds: – Continental Glaciers – Valley Glaciers.
Glaciers. “ RIVERS OF ICE ” Mass movement of frozen ice on land Mass movement of frozen ice on land Form at high elevations or high altitude Form at high.
South Island, New Zealand February 2005 Katherine Ihli and Glen Liston.
D. Evan Stribling  a larger mass of compacted snow and ice that moves under the force of its own gravity (weight)  They erode in some places deposit.
Features of erosion and deposition associated with glaciated landscapes Moving Ice.
Glaciers once covered most of the Earth –in total there have been up to 22 times when glaciers covered large areas of the Earth… including Alberta the.
Agenda Check In Review notes Glaciers WATER Who’d’a Thunk: Karaoke means “empty orchestra” in Japanese.
Like running water, gravity is the driving force
Chapter 7.1 Glaciers  A glacier is a thick ice mass that forms above the snowline over hundreds or thousands of years. • The ice age was a period of.
An agent of erosion, weathering, and deposition
Chapter 8 – Mass movements, Wind and Glaciers
Presentation transcript:

Dry Valleys, Antarctica 77°00' S Latitude 162°52' E Longitude (31 December 2004 – 3 February 2005)

Christchurch, New Zealand

Clothing issue in Christchurch

C-141 Starlifter Transport to Antarctica

The 5.5 hour flight to Antarctica (not fun)

Landing on the Ice Shelf

Transport to McMurdo Station

McMurdo Station

Mount Erebus

Helicopter ride to the Dry Valleys

Taylor Valley (Photo courtesy of Mike Prentice;

Lake Hoare Camp

Research Labs

Solar Power for Station

Tents To Sleep In

High-Tech Outhouses

ALL waste is shipped out to the US.

Andrew Fountain The Team Glen Liston

Jon EbnetThomas Nylen

Our goal is to understand how sediment on the glacier influences glacier melt.

Each glacier has different sediment loads and surface characteristics.

Sea Ice Ice Bergs Lake Ice Glacier Snow

We either flew or walked to our research sites/glaciers.

The presence of sediment has a huge influence on melt rates.

Dirt melting into the ice.

The melt features can be very large.

Melt walls 10 m (30 ft) tall.

The melt finds its way into valley streams.

The stream discharge is measured throughout the Dry Valleys.

The present glacier over-riding an old lateral moraine.

A glacier calving study.

These glacier walls are very impressive.

Helicopter Operations

Mass balance measurements on the Taylor Glacier.

Interesting Geology

More Helicopter Operations

Mummified seals, up to 3500 years old.

Meteorological Station Maintenance

Ventifacts, caused by abrasion of wind-blown grit.

Permafrost, Ice-Wedge Polygon Study

The lakes in the Taylor Valley are generally covered by very dirty ice that is a few meters thick.

A dirty, ice-covered lake, with a research hut.

Like the glaciers, the sediment plays a large role in the lake-ice melt.

Re-freezing of the lake moat.

Lake Ice Melt

Algal mats (under water), showing sand underneath, and oxygen bubble production.

Orange-colored algal mats, with ice above that contains bubbles from algal productivity.

Otherwise, a visibly dry, and unvegetated landscape.

The glaciers are truly amazing!

We head back to McMurdo.

Penguins

Mutton

Time to head back to Christchurch.

Dreaming of vegetation.

The End