KITSAP COUNTY
Kitsap county is essentially a peninsula, situated between Hood's canal on the west and the main body of Puget Sound on the east. Its shores are greatly indented, abounding in good harbors, so that much of the transportation of the county is carried on by water. It is located within the Puget Sound
[Source: Bulletin No. 2, By Washington Geological Survey, Washington (State). Division of Geology, Washington (State). Geology and Earth Resources Division, Published by 1911 - Submitted by K. Torp]
lowland, so that no part of its gently rolling surface exceeds 600 feet above the sea. It was once heavily forested but the virgin timber is now largely removed. Because of its proximity to good markets the logged-off lands are being cleared for farms. The farms are generally small so that in certain localities the rural population has grown to the point where good roads are now necessary. As a rule the roads are short, extending from the interior of the peninsula to the nearest good harbor where there are wharves.
The major part of the county is deeply buried under a thick mantle of glacial sediments. The highways so far have been entirely made of these materials. The glacial till, composed of pebbles with a cement of clay, makes a fair road wherever the drainage and the grades are good. It is likely to be very dusty in summer and muddy in winter. Beds of gravel are generally distributed, as a part of the glacial deposits, and may be used in surfacing the highways. Bedrock appears at the surface but rarely and then usually about the shores of the Sound or along Hood's canal. It is prevailingly sedimentary in character, usually alternating layers of sandstone and shale. It is worthless as a source of road materials. Basalt is very scarce and the locality described below is the only well known accessible one. Igneous dikes occur in the low hills west of Chico but not in a convenient location for use in road building.
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