• Refine Query
  • Source
  • Publication year
  • to
  • Language
  • 186
  • 26
  • 19
  • 6
  • 6
  • 4
  • 1
  • 1
  • 1
  • 1
  • 1
  • 1
  • 1
  • 1
  • 1
  • Tagged with
  • 296
  • 58
  • 51
  • 49
  • 34
  • 33
  • 33
  • 30
  • 26
  • 26
  • 22
  • 22
  • 20
  • 20
  • 16
  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
71

Holocene glacier fluctuations around Eyjafjallajökull, south Iceland : a tephrochronological study

Dugmore, Andrew J. January 1987 (has links)
Stratigraphic studies of layers of volcanic ash, or tephra, in buried soils have been used to date accurately Holocene glacier fluctuations in Southern Iceland. 132 stratigraphic sections up to 11m deep, and containing up to 78 tephra layers, were logged to a resolution of 0.25cm. The chronological framework was completed with 12 radiocarbon dates, and by examing the association of the tephra stratigraphy with moraines representing former ice margins, a chronology of Holocene glacier fluctuations was constructed. The forelands of five glaciers were studied: Seljavallajokull, Gigjokull and Steinholtsjokull (outlets of Eyjafjallajokull) and Solheimajokull and Klifurarjokull (outlets of Myrdalsjokull). This study has shown for the first time that large glaciers existed in mid-Holocene Iceland because after 700 BP and before 4500 BP Solheimajokull extended at least 4km beyond its present limits, and terminated at less than 100m above sea level. Other major advances of this glacier culminated before 3100 BP, and between 1400-1200 BP. In the tenth century AD Solheimajokull was also longer than during the late Little Ice Age (1700-1900 AD). In contrast, Klifurarjokull and all the outlets of Eyjafjallajokull reached a maximum Holocene extent during the late Little Ice Age. It is proposed that the anomalous behaviour of Solheimajokull may be explained as a result of catchment changes caused by the growth of the Myrdalsjokull ice cap. The great human impact on the landscape since the Norse Settlement (c870-930 AD) has also been assessed as a result of the extensive study of the aeolian sediments lying between numerous, accurately dated tephra layers. These studies show that a zone of chronic soil erosion developed in the natural upland pastures immediately after the Norse Settlement and slowly swept down hill to reach lowlying areas during the last 400 years.
72

Interpretation of glaciochemical records from an array of Greenland ice cores

Banta, John Ryan. January 2006 (has links)
Thesis (Ph. D.)--University of Nevada, Reno, 2006. / "August, 2006." Includes bibliographical references. Online version available on the World Wide Web.
73

Biogeography of holocene bison in the greater Yellowstone ecosystem

Cannon, Kenneth P. January 1900 (has links)
Thesis (Ph.D.)--University of Nebraska-Lincoln, 2008. / Title from title screen (site viewed Aug. 12, 2008). PDF text: x, 249 p. : ill. (some col.), maps (some col.) ; 11 Mb. UMI publication number: AAT 3297752. Includes bibliographical references. Also available in microfilm and microfiche formats.
74

Past climate variability in southwestern Oregon and relationships with regional and hemispheric climate /

Ersek, Vasile. January 1900 (has links)
Thesis (Ph. D.)--Oregon State University, 2009. / Printout. Includes bibliographical references (leaves 94-101). Also available on the World Wide Web.
75

Petrography and discontinuities, growth rates and stable isotopes of speleothems as indicators of paleoclimates from oregon Caves National Monument, southwestern Oregon, USA.

Turgeon, Steven Charles, January 1900 (has links)
Thesis (Ph. D.)--Carleton University, 2001. / Also available in electronic format on the Internet.
76

Palaeoenvironments of the Gulf of Carpentaria from the last glacial maximum to the present, as determined by foraminiferal assemblages

Holt, Sabine. January 2005 (has links)
Thesis (Ph.D.)--University of Wollongong, 2005. / Typescript. Includes bibliographical references: leaf 215-246.
77

High precision TIMS U-Th disequilibrium dating and C, O, Sr isotope-based multi-proxy palaeoclimatic study of Speleothems in Australia /

Xia, Qikai. January 2004 (has links) (PDF)
Thesis (Ph.D.) - University of Queensland, 2005. / Includes bibliography.
78

Objective reconstruction of the paleoclimatic record through application of eigenvectors of present-day pollen spectra and climate to the late-quarterary pollen stratigraphy

Cole, Henry S. January 1969 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison, 1969. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliography.
79

Geochemical tools and paleoclimate clues : multi-molecular and isotopic investigations of tropical marine sediments and alpine ice /

Makou, Matthew C. January 2006 (has links)
Originally issued as the author's thesis (Ph. D.)--Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2006. / "February 2006". "Doctoral dissertation." "Department of origin: Geology and Geophysics." "Joint Program in Oceanography/Applied Ocean Science and Engineering"--Cover. Includes bibliographical references.
80

Late Holocene climate variability as preserved in high-resolution estuarine and lacustrine sediment archives /

Hubeny, Jeremiah Bradford. January 2006 (has links)
Thesis (Ph. D.)--University of Rhode Island, 2006. / Typescript. Includes bibliographical references (leaves 220-239).

Page generated in 0.0373 seconds