Feature: Arctic Thaw

Measuring Change

Witnessing time – from 445 million year old rocks exposed in the Fjords to ~4 thousand year old small ice caps

by | 5.15.2011 at 11:09am | 2 Comments
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The IceBridge P3 (photo H. Abdi)

By Hakim Abdi, LDEO.
My first flight on the P3 and the scenery was nothing short of breathtaking. The science mission involved flights in the north over the Steensby glacier that passes through Sherard Osbron Fjord, and Ryder glacier constrained by the Victoria Fjord. In northeast Greenland we overflew the Hagen glacier and the Flade Isblink Ice Cap in Kronprins Christian Land.

Northern Glacier Flight Plan - main areas of interest are the northernmost and northeasternmost loops (image NASA IceBridge Program)

The sheer dimensions of the fjord cliffs on the northern flights were striking. In north Greenland they were quite steep, at almost 90 degrees, and appeared to be carved with surgical precision. Formed in the last glacial period as Greenland was covered with ice and snow, the weight of the ice depressed the crust and glaciers cut through surrounding rock. Since the end of the last ice age, a phenomenon called ‘crustal rebound’ has taken place. The formerly depressed land masses have slowly risen in a process is called isostasy, resulting in these awe-inspiring cliffs.

Middle Ordovician – Lower Silurian cliffs (~445 million years old) surround the Sherard Osborn Fjord and the Victoria Fjord (Photo H. Abdi)

Outside the scientific community, glaciers are sometimes thought of as ‘just a block of ice’, but they are much like landmasses in their own right, close to inland islands. They are solid, yet they are dynamic, with internal layers that record events during the lengthy history of their formation. They also have surficial features, including crevasses, such as those shown below. Crevasses are deep cracks in the ice sheet, equivalent to fractures in rock, and are formed due to a combination of factors including differences in the ice speed between the edges and center of the glacier, stresses generated by flow over an uneven terrain, and the stress created from the glacier’s lower layers being more malleable than its upper layers.

Crevasses forming on the Ryder Glacier. The photo does not give justice to scale. These features are easily 100m wide. (photo H. Abdi)

In Northeast Greenland we focused on the Hagen glacier and the Flade Isblink icecap. Like the flights over the northern glaciers we are resurveying historical ATM lines. Flade Isblink is a small, ~600 m thick, icecap in the furthermost northeast corner of Greenland located just south of Station Nord (a permanently occupied Danish scientific and military base) in Kronprins Christian Land. Flade Isblink faces the Polar Ocean and is separated from the central ice sheet so the age of the ice in this small icecap was recently determined to be much younger than the main icesheet. An ice core drilled by the Centre for Ice and Climate, Copenhagen University, suggests the age of this small ice cap to be between 2800 -4000 yrs (A. Lemark, 2010).

Kronprins Christians Land, a peninsula named after the Danish Crown Prince (later king) Christian the X (photo Hakim Abdi)

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2 Responses to “Witnessing time – from 445 million year old rocks exposed in the Fjords to ~4 thousand year old small ice caps”

  1. Beautiful pictures, but your headline writer needs to learn the difference between 4000 years and 4000 thousand (= 4 million) years. And the fjords aren’t 445 million years old; the rocks in which they are carved are.

  2. Kirsty Tinto says:

    Yes changed the title to reflect the age being of the exposed rocks on the fjords. Thanks. However, the ~4 thousand year age on the ice cap is correct (see linked reference).

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