936 resultados para Berkshire Hills
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Belleville East, 1908: Map of the Huron River Valley. [Scanned in two parts and combined using PhotoShop CS6 PhotoMerge command. The number "5110" is in pencil on the edges of the drawing, and the word "old" is in pencil is written in the lower right corner of the map.]
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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"A sermon, delivered... August 22, 1844... By Mark Hopkins, D.D.": p. [29]-62; "An oration... August 23, 1844. By J. A. Spencer": p. [107]-132; "A recollection of the Stockbridge Indians. By Thomas Allen": p. [197]-205; "Catalogue of Berkshire soldiers and chaplains in the French and revolutionary wars": p. 211-213; "Names of emigrant sons": p. [233]-242.
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Mode of access: Internet.
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Mode of access: Internet.
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Title varies: 1911-22, The Pahasapa Quarterly
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Mode of access: Internet.
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Mode of access: Internet.
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This report presents the results of stratigraphic analysis of the southwestern quadrant of the Cedar Hills Regional Landfill (CHRLF). My report was intended to incorporate the recent Area 8 borehole data into the pre-existing analyses. This analysis was conducted during the preparation of the Area 8 Hydrogeologic Report, but is my independent investigation and does not represent the opinion of UEC or their associates. The CHRLF, in Maple Valley, WA, south of Squak Mountain, is a municipal solid waste landfill that has been in operation since the 1960s. A network of borings, the product of previous investigations, exists for the study area. I utilized the compiled boring logs, previous investigations, and the recently acquired data to produce a series of interpretative cross-sections for the study area. I recognized 9 distinct stratigraphic units, including fill. My interpreted stratigraphic units are similar to those identified in previous investigations such as the Area 7 Hydrogeologic investigation (HDR Engineering and Associates, 2008). These units include pre-Olympia aged non-glacial alluvium, glacial alluvium, and glacial till. Additionally, younger, Vashon-aged deposits of glacial till, recessional outwash, recessional lacustrine, and ice-contact were observed. An isolated “till-like” deposit was observed below the Vashon till. This could possibly represent an older till as mapped by Sweet Edwards (1985) and Booth (1995). I cite the continuity of the lower contact of the Vashon till (Unit 5, Table 2) and the upper contact pre-Vashon non-glacial fluvial deposits (Unit 9, Table 2) as evidence that faults or other structural features do not offset the deposits in the study area. This conclusion supports the findings of the pre-existing body of work within the landfill property and the nearby Queen City Farms property.