Vote of the Corporation continuing the salary of the President up to the next commencement,

This folder contains two nineteenth-century handwritten copies of the vote.

Vote of the Corporation accepting Kirkland's resignation,

This folder contains a nineteenth-century handwritten copy of the vote.

Answer to vote of Corporation,

This folder contains a nineteenth-century copy of Kirkland's original letter.

Copies of papers relating to the resignation of President Kirkland of Harvard University,

This folder contains a notebook that includes handwritten copies of Kirkland's letter of resignation addressed to the Corporation of Harvard University, March 28, 1828; an address of President Kirkland to the students, delivered in the College Chapel after morning prayers, April 1, 1828; a letter from Francis C. Gray accompanied by a vote of the Corporation, April 2, 1828; a letter from Mr. Gray and vote of the Corporation, April 4, 1828; President Kirkland's reply to Mr. Gray, April 5, 1828; the address of the senior class to the President, presented to him the morning after he took leave of the College, April 2, 1828; and an address of the immediate government to Kirkland, April 2, 1828.

Letter from Samuel Willard, Harvard College, Cambridge, Massachusetts, to Sophronia Willard, Lancaster, Massachusetts, October 18, 1805

Willard describes his current job working at Harvard, where he is paid “to keep order in one of the buildings.” He mentions that he can attend medical lectures free of charge, and refers to a preacher, Mr. Parker, a former classmate of Willard’s. He explains that he is currently with his brother Solomon, who is ill, and that he is living in the College House, where he resided his first year of school.

New England and Eastern New York Railroads, 1849 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Railroad map of New England & eastern New York : compiled from the most authentic sources, by J.H. Goldthwait. It was published in 1849 by Redding & Co. and Clark, Austin, & Co. Scale [ca. 1:700,000]. Covers Massachusetts, Rhode Island, Connecticut, and portions of New York, Vermont, New Hampshire, and Maine. The image inside the map neatline is georeferenced to the surface of the earth and fit to the USA Contiguous Albers Equal Area Conic projection (Meters). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows features such as railroads completed and in progress, drainage, state, county, and town boundaries, and more. Includes inset: Boston & vicinity showing the Grand Junction R.R. Scale [ca. 1:170,000]. This layer is part of a selection of digitally scanned and georeferenced historic maps of New England from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Core correlation data and revised composite depth scale of Exp302 (ACEX) cores

Expedition 302 of the Integrated Ocean Drilling Program (IODP), also known as the Arctic Coring Expedition (ACEX), successfully penetrated a sequence of Cenozoic sediments draping the crest of the Lomonosov Ridge in the central Arctic Ocean. The cumulative sedimentary record spans the last 57 m.y. and was recovered from three sites located within 15 km of each other. Merging the recovered cores onto a common depth scale that accurately reflects their stratigraphic placement below the seafloor is a fundamental step toward interpreting this unique sedimentary record. However, the lack of overlapping recovery in adjacent holes and intervals of high core disturbance complicated traditional methods of stratigraphic correlation. Here we present a revised composite depth scale for the ACEX sediments, generated in part by performing a regional stratigraphic correlation with sediments recovered from previous expeditions to the Lomonosov Ridge. The revised depth scale also reassesses the offsets for cores in the upper 55 meters below seafloor, where no overlapping recovery was acquired, and proposes modifications to these depths.

Sedimentological and paleomagnetic investigations on two gravity cores and ODP sites 113-690 and 693 off Kapp Norvegia, Antarctic continental margin

Oligocene to Quaternary sediments were recovered from the Antarctic continental margin in the eastern Weddell Sea during ODP Leg 113 and Polarstern expedition ANT-VI. Clay mineral composition and grain size distribution patterns are useful for distinguishing sediments that have been transported by ocean currents from those that were ice-rafted. This, in turn, has assisted in providing insights about the changing late Paleogene to Neogene sedimentary environment as the cryosphere developed in Antarctica. During the middle Oligocene, increasing glacial conditions on the continent are indicated by the presence of glauconite sands, that are interpreted to have formed on the shelf and then transported down the continental slope by advancing glaciers or as a result of sea-level lowering. The dominance of illite and a relatively high content of chlorite suggest predominantly physical weathering conditions on the continent. The high content of biogenic opal from the late Miocene to the late Pliocene resulted from increased upwelling processes at the continental margin due to increased wind strength related to global cooling. Partial melting of the ice-sheet occurred during an early Pliocene climate optimum as is shown by an increasing supply of predominantly current-derived sediment with a low mean grain size and peak values of smectite. Primary productivity decreased at ~ 3 Ma due to the development of a permanent sea-ice cover close to the continent. Late Pleistocene sediments are characterized by planktonic foraminifers and biogenic opal, concentrated in distinct horizons reflecting climatic cycles. Isotopic analysis of AT. pachyderma produced a stratigraphy which resulted in a calculated sedimentation rate of 1 cm/k.y. during the Pleistocene. Primary productivity was highest during the last three interglacial maxima and decreased during glacial episodes as a result of increasing sea-ice coverage.