But there is another and more dangerous ice than floe ice, as it takes many years for its formation. It is met with in isolated floes, but rarely if ever in pack below Smith's Sound, and the Scotch whalers seldom encounter it. Ships have been nipped hundreds of times in floe ice and escaped, but few if any have ever freed themselves from the fierce grasp of the ancient ice of the arctic, called by Nares floe-berg or Paleocrystic ice. This bears evidence of great age, the part above water being from fifteen to forty-five feet in thickness, which would make its depth from one hundred and thirty-five to four hundred and five feet ; the stout- est-built ship that ever put to sea would be crushed into match- sticks by the pressure of two such floes upon her sides. This ice forms the northern limit of the cruising-grounds of the American whalers north of Alaska. Some years it moves to the southward and closes up on them ; again, it recedes, disclosing more of the mystery of the farther north. Scattered here and there through it are yohjnias, or lakes of ice, of one year's growth, enclosed by heavy floes arched and keyed together.
Paleocrystic ice is old pack ice built up by successive deposits of snow during a long period of time, thus giving it an appear- ance of stratification. There is an alternation of soft white and hard blue ice, representing, respectively, compressed snow and water formed during the sunshine by thaws, and frozen at night or when cloudy. (It is a remarkable fact that snow will melt and seep through floe ice in sunlight though the thermometer may record far below the freezing-point.) Eventually, during the long summer day, the floe is left bare and dry, but soft and porous, unless so far north that the snow-storms continue all the year round. Over some strata are layers of atmospheric dust, such as Nordenskiold found on the Greenland glaciers ; also the gradual decrease of the thickness of the layers — due to pressure and in- crease of blue ice — because of greater infiltration, as the lower part of the berg is approached, make certain the progressive nature of the formation.
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Dug this out of;
http://en.wikisource.org/wiki/Page:Popular_Science_Monthly_Volume_35.djvu/701
to let folk read about the old 'Paleocrystic ice' that used to form the 'backbone' of the Arctic ice pack and formed most of the sea ice come ice min in Sept.
Sadly the last of this ice type disappeared in South Beaufort last July and ,with the mixing out of the halocline, the conditions that allowed it to be no longer exist in the Arctic Basin
Koyaanisqatsi
ko.yaa.nis.katsi (from the Hopi language), n. 1. crazy life. 2. life in turmoil. 3. life disintegrating. 4. life out of balance. 5. a state of life that calls for another way of living.
VIRESCIT VULNERE VIRTUS