999 resultados para Saginaw, Michigan
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Letter to S.D. Woodruff from J.J.B. at the National Hotel in East Saginaw, Michigan. The writer informs Mr. Woodruff that there is about 26,000 of first class board pine which was cut. Mr. Woodruff did not give a receipt to Barton and Bro., Jan. 20, 1880.
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Letter (1 handwritten, double sided page) to S.D. Woodruff from J.J.B. in Saginaw, Michigan. J.J.B. says that he doesn’t want any money for his information. He explains where the pine is, and encloses a crudely drawn map. He says the Mr. Woodruff can correspond with him, but to please keep this a secret, Jan. 23, 1880.
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Mode of access: Internet.
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"Lake Belnona" was built at Saginaw, Michigan in 1918 by the Saginaw Shipbuilding Company. She was owned by the U. S. Shipping Board of Washington, D. C. until 1928 when she was scrapped at River Rouge, Michigan by the Ford Motor Company
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We identified, mapped, and characterized a widespread area (gt;1,020 km2) of patterned ground in the Saginaw Lowlands of Michigan, a wet, flat plain composed of waterlain tills, lacustrine deposits, or both. The polygonal patterned ground is interpreted as a possible relict permafrost feature, formed in the Late Wisconsin when this area was proximal to the Laurentide ice sheet. Cold-air drainage off the ice sheet might have pooled in the Saginaw Lowlands, which sloped toward the ice margin, possibly creating widespread but short-lived permafrost on this glacial lake plain. The majority of the polygons occur between the Glacial Lake Warren strandline (~14.8 cal. ka) and the shoreline of Glacial Lake Elkton (~14.3 cal. ka), providing a relative age bracket for the patterned ground. Most of the polygons formed in dense, wet, silt loam soils on flat-lying sites and take the form of reticulate nets with polygon long axes of 150 to 160 m and short axes of 60 to 90 m. Interpolygon swales, often shown as dark curvilinears on aerial photographs, are typically slightly lower than are the polygon centers they bound. Some portions of these interpolygon swales are infilled with gravel-free, sandy loam sediments. The subtle morphology and sedimentological characteristics of the patterned ground in the Saginaw Lowlands suggest that thermokarst erosion, rather than ice-wedge replacement, was the dominant geomorphic process associated with the degradation of the Late-Wisconsin permafrost in the study area and, therefore, was primarily responsible for the soil patterns seen there today.
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"Concluded at Isabella ... Michigan."
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Two leaves (one not numbered, the other numbered 105-106) inserted between p. 108 and p. 109.
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Mode of access: Internet.
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Mode of access: Internet.
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Includes index.
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Mode of access: Internet.
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Shipping list no.: 94-0331-P.
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"This Catalogue is printed by the State of Michigan and contains a list of products manufactured by the State at the Michigan Employment Institution for the Blind at Saginaw and the State Prisons at Jackson, Ionia and Marquette."--P. 3.