Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Civil Engineering, 1977. / MICROFICHE COPY AVAILABLE IN ARCHIVES AND ENGINEERING. / Bibliography: leaves 150-160. / Ph.D.

Thesis (Ed.M.)--Boston University / PLEASE NOTE: Boston University Libraries did not receive an Authorization To Manage form for this thesis or dissertation. It is therefore not openly accessible, though it may be available by request. If you are the author or principal advisor of this work and would like to request open access for it, please contact us at open-help@bu.edu. Thank you. / 2031-01-01

Thesis. 1979. M.Arch.--Massachusetts Institute of Technology. Dept. of Architecture. / MICROFICHE COPY AVAILABLE IN ARCHIVES AND ROTCH. / M.Arch.

Boston University. University Professors Program Senior theses. / PLEASE NOTE: Boston University Libraries did not receive an Authorization To Manage form for this thesis. It is therefore not openly accessible, though it may be available by request. If you are the author or principal advisor of this work and would like to request open access for it, please contact us at open-help@bu.edu. Thank you. / 2031-01-02

Thesis (M.B.A.)--Boston University

Thesis (Ed.M.)--Boston University

Thesis (Ph. D.)--University of Georgia, 1999. / Directed by Thomas C. Reeves. Includes bibliographical references (leaves 198-214).

Thesis (Ph. D.)--University of Pennsylvania, 1917. / Reprinted from the Bulletin of the Geographical society of Philadelphia, vol. xv, no. 3, July, 1917; vol. xv, no. 4, October, 1917. Caption title: Some responses to environment in Massachusetts.

The study area encompasses 1100 km('2) in northwestern Connecticut and adjacent Massachusetts. It contains three lithologic-topographic belts: a crystalline upland, a marble lowland, and a phyllitic upland; each having two tills, the youngest of Woodfordian age. The youngest or "upper" till has ablation, resedimented (diamicton), meltout and basal facies. The older or "lower" till has oxidized and unoxidized zones. Tills and till facies of each belt can be discriminated by grain size and clast weathering characteristics. Abundance isopleths of upper till heavy minerals and exotic clasts indicate strong topographic control of basal ice movement and possible glaciotectonic thrusting. Field relationships and upper till compositional changes in the crystalline belt suggest this sequence: (1) erosion of the bed, (2) lodgment of till, (3) erosion of the bed and reincorporation of previously deposited till, and (4) ice stagnation. Entrained subglacial material locally was frozen during (3).

Thesis (Ph. D.)--University of Pennsylvania, 1917. / Reprinted from the Bulletin of the Geographical society of Philadelphia, vol. xv, no. 3, July, 1917; vol. xv, no. 4, October, 1917. Caption title: Some responses to environment in Massachusetts.