Monday, 20 November 2000

Friday, 20 October 2000

Cedar: Lifeblood to an Island


Tsyyaaay: The arrival of cedar, called “Tsuuaay” by the Haida, had profound effects on the material culture of the Haida (Approx 4000 BC). Once they were able to build canoes to fish year round (Halibut, Red Snapper, Ling Cod etc) and could access sea mammals, they no longer only depended on the salmon to return at certain times. The cedar bent wood box, a genius idea in food conservation and storage, allowed them to store food for the winter and reduced their dependence on hunting land mammals throughout the year wained.


Birth of a New Tradition: The arrival of cedar marked a whole new stone tool tradition. The micoblades are abandoned for larger ground tools, which are more appropriate for working with cedar.

LICHTKASTEN :: EXQUISITE DECAY

Tuesday, 11 July 2000

Tuesday, 4 July 2000

Thursday, 29 June 2000

PALEONTOLOGY AND GEOLOGY OF WASHINGTON

The Precambrian: Precambrian rocks exist only along the northeastern portion of the state. Since the Precambrian, huge amounts of crust have been added to the western edge of the North American continent.

All the land west of the Precambrian rocks has been created through complex tectonic processes along an active continental margin or transported from elsewhere and accreted onto the continent of this region.

Paleozoic: In the early Paleozoic, easternmost Washington was at the edge of a large ocean. Early Paleozoic fossiliferous sandstone, shales, and limestone were deposited along this ancient shoreline.

Other Paleozoic sedimentary rocks of Washington were transported as exotic terranes and accreted to the margin of the continent in the Mesozoic. These terranes contain unrelated slivers of Devonian-, Carboniferous-, and Permian-aged rocks, originally formed far from their present location.

Mesozoic: During the late Jurassic and early Cretaceous, numerous blocks of exotic terranes were added to the western edge of the North American continent to form most of what we know as Washington state today. British Columbia and Oregon are also made up primarily of these terranes. Most of these terranes consist of narrow, banded,rock sequences, often overturned and formed far from their current location —much like a badly shuffled deck of cards.

They include volcanic island rocks and fossiliferous marine sediments that originated elsewhere in the Pacific Ocean. Jurassic and Cretaceous fossils occur in the north-central and northwestern part of the state. By the end of the Mesozoic, approximately two-thirds of the state was assembled.

Cenozoic: Cenozoic marine sediments make up the western part of Washington and were formed as the sea gradually retreated westwards. Marine fossiliferous sandstones and siltstone cover most of Washington west of the Cascades Mountains.

The Olympic Mountains consist of marine sedimentary rocks uplifted about 10 million years ago. The Cascade volcanic began in the mid-Cenozoic and has been active ever since. Continental sedimentary rocks are not common. Continental ice sheets covered the northern third of the state during the late Cenozoic, and alpine glaciers covered the Cascades and Olympic Mountains. Large and small mammals lived at the edge of the ice, and salmon swam up the rivers to ice-blocked dams.

From the paleontological portal: http://www.paleoportal.org/kiosk/sample_site/state_46.html

Monday, 29 May 2000

Wednesday, 24 May 2000

Friday, 21 April 2000

Thursday, 3 February 2000

Thursday, 27 January 2000