Receipt for items shipped by Gardner and Clark

Receipt for items shipped by Gardner and Clark for lake freight which was received in St. Catharines on July 18, 1876. This is signed by John Cassidy, July 10, 1876.

Acceptance of the Clark P. Read Mentor Award: The Teague Self Lessons

The transcript of John J. Janovy Jr.'s speech upon acceptance of the American Society of Parasitologists' Clark P. Read Mentor Award, 2003.

John Basset

http://commons.clarku.edu/mosakowskiinstitute_gallery/1003/thumbnail.jpg

Geology and Ore Deposits of the Golden Messenger MIne, Lewis and Clark County, Helena, Montana.

The Golden Messenger Mine which is approximately twenty-three miles northeast of Helena, Montana, near York, on Trout Creek, has long presented several problems of both theoretical and practical interest.

(Table 3) Sedimentation rates of stage 1 and last glacial maximum from different Holes during cruises of RRS Discovery in 1984-1985 and 1987-1988, and RRS James Clark Ross in 1992-1993

Within the Scotia Sea, the axis of the Antarctic Circumpolar Current (ACC) is geographically confined, and sediments therefore contain a record of palaeo-flow speed uncomplicated by ACC axis migration. We outline Holocene and Last Glacial Maximum (LGM) current-controlled sedimentation using data from 3.5-kHz profiles, cores and current meter moorings. Geophysical surveys show areas of erosion and deposition controlled by Neogene basement topography. Deposition occurs in mounded sediment drifts or flatter areas, where 500-1000 m of sediment overlies acoustic basement. 3.5-kHz profiles show parallel, continuous sub-bottom reflectors with highest sedimentation rates in the centre of the drifts, and reflectors converging towards marginal zones of non-deposition. Locally, on the flanks of continental blocks (e.g. South Georgia), downslope processes are dominant. The absence of mudwaves on the sediment drifts may result from the unsteadiness of ACC flow. A core transect from the ACC axis south to the boundary with the Weddell Gyre shows a southward decrease in biogenic content, controlled by the Polar Front and the spring sea-ice edge. Both these features lay farther north at LGM. The cores have been dated by relative abundance of the radiolarian Cycladophora davisiana, and by changes in the biogenic Ba content, a palaeoproductivity indicator. Sedimentation rates range from 3 to 17 cm/ka. The grain size of Holocene sediments shows a coarsening trend from south to north, consistent with strongest bottom-current flow near the ACC axis, though interpretation is complicated by the presence of biogenic grains. Year-long current meter records indicate mean speeds from 7 cm/s in the south to 12 cm/s in the north, with benthic storm frequency increasing northwards. LGM sediments are predominantly terrigenous and show a clearer northward-coarsening trend, with well-sorted silts in the northern Scotia Sea. Assuming a constant terrigenous source, this implies stronger ACC flow at the LGM, contrasting with weaker Weddell Gyre flow deduced from earlier work.

John Oldham counterbond to James Clarke & Richard Moores, 1722 May 14

This legal document, a counterbond, was created on May 14, 1722 and involved John Oldham, James Clark, and Richard Moores. All three men were residents of Cambridge at the time of its creation. The document specifies Oldham's financial obligations to Clark, a cordwainer, and Moores, a tailor and was "Sign[ed], sealed & [delivered] in the presence of Nathaniel Sparhawk and Noah Sparkhawk." The document also refers to the "trustees for the town of Cambridge" Spencer Shipps, Nathaniel Sparhawk and John Dickson.

In memoriam. Josiah Clark, LL.D., principal of Williston Seminary 1849-1863. : Obiit [sic] May 30, 1878. /

"Published by the Trustees of Williston Seminary, for gratuitous distribution among the Alumni, and other friends of Williston Seminary"--T.p. verso.

"Brief lives", chiefly of contemporaries, set down by John Aubrey, between the years 1669 & 1696;

v. 1. A-H.--v. 2. I-Y.