James Otis research materials,

Includes copies of correspondence from James Otis, and copies of historical summaries of the Stamp Act and extracts from the annual register, circa 1760s.

James Otis research materials,

Includes extracts from Benjamin Franklin’s works.

James Otis research materials,

Includes notes on activities of the Stamp Act Congress in 1765.

James Otis research materials,

Includes copies of correspondence from James Otis, notes on the American Revolution, and an extract from the Journal of Congress, approximately 1760s-1780s.

James Otis research materials,

Draft of Tudor’s manuscript, interfiled with loose notes and extracts from John Reeves’ work on English law, and a copy of Otis’ supposed work, "An Appeal to the World, or, a Vindication of the Town of Boston," approximately 1760s-1820s.

James Otis research materials,

Draft of Tudor's manuscript, interfiled with loose notes and copies of various documents regarding the Boston Tea Party and the Charter Oak tree.

James Otis research materials,

Notes for a chapter that included the history of two pieces of artillery, the "Adams" and the "Hancock," used in Revolutionary War; epitaph in Latin on William Bollan, and agent for the province of Massachusetts, and Governor William Shirley; clippings regarding the death of General James Warren.

James Otis research materials,

Undated copied and original correspondence and remembrances of James Otis.

(Table A1) Calcium carbonate content of boreholes Kirchrode I and II

The technical details of drilling and coring at the Kirchrode I and II sites are presented. At these sites, a sequence of claystones and marlstones from an Albian shelf basin was recovered. Constraints on the ages of the sediments in the two boreholes are provided by the occurrence of the inoceramid bivalve Actinoceramus sulcatus, the first appearance of which is used to define the Middle/Upper Albian boundary and by observed facies changes that can be correlated to the established lithostratigraphy. The cores from the two boreholes provide a rather complete, 285-m-long sequence of the Upper Albian, with a 155.5-m-long overlap. Analysis of the tectonic structures showed considerable shortening in the Middle and Lower Albian part of the sequence due to normal faulting. Of the Upper Albian, only the lowermost part is affected by faults. The increase in sedimentation rates of terrigenous detritus and of marine biogenic carbonate, which occurs in the basal part of the C. auritus Subzone, is interpreted to reflect a regional change to a more humid climate and regional tectonic movements (uplift of the Rhenish Bohemian massif, subsidence of the Lower Saxony basin intensified locally by halokinetic movements). The further increase in marine productivity in the latest Albian may be related to upwelling of more nutrient-rich deep water along submarine relief in this shelf sea. Identification of Milankovitch cyclicity documented by the fluctuating CaCO3 contents of the sediments is used (i) to constrain the minimum time represented by the Upper Albian deposits, and (ii) to determine the duration of the sea level cycles (Cycle V: >=1.6 Ma, Cycle VI: >=2 Ma), and (iii) to establish the duration of the Late Albian ammonite subzones (e.g. Callihoplites auritus Subzone: 2.1 Ma). Average sedimentation rates determined from the identified 100-ka eccentricity cycles show a stepwise increase in sedimentation rates from 1-2 cm/1000 a in the Lower Albian dark claystones to 7-13 cm/1000 a in the late Late Albian. In addition to the general deepening trend through the Late Albian, two, nearly completely documented 3rd-order sea-level cycles in the Upper Albian of Kirchrode I were recognised, plus another one, cut short by faulting, at the base of the Upper Albian (documented in Kirchrode II). These global sea-level cycles were identified on the basis (a) of the sequence of the abundance maxima of selected benthos and plankton groups, (b) of trends in the fluctuations of the CaCO3 content, and (c) of the abundance of glauconite. The transgression periods in this Upper Albian deep shelf-basin are characterised by intensified circulation. This intensified circulation is found to have affected first the surface-near waters, resulting e.g. in an increase in the abundance of immigrant plankton and nekton species from the Tethys. At a later stage the deep water was affected, supporting then an increased population of suspension-feeding benthos, and causing condensation and erosion in the sediment at the sea floor.

Improved commercial vehicle conspicuity and signalling systems. Task II: analyses, experiments and design recommendations. Interim report.

National Highway Traffic Safety Administration, Washington, D.C.

Development of a test methodology for evaluating crash compatibilities and aggressiveness. Volume II: technical report. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Technology assessment of automotive applications of metal-plastic laminates. Volume II. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

The development of a classification scheme for brake linings. Volume II. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Crash padding research. Volume II: constitutive equation models. Final report.

National Highway Traffic Safety Administration, Office of Research and Development, Washington, D.C.