A GIS method for reconstruction of late Quaternary landscapes from isobase data and modern topography

Computers and Geosciences

Volumn 28, Issue 5, 2002, Pages 631-639

  Leverington, David W ^a,b   Teller, James T ^a   Mann, Jason D ^a  

^a UNIVERSITY OF MANITOBA   (Canada)

^b DEPARTMENT OF PALEOBIOLOGY   (United States)

Author keywords

Geographic information system (GIS); Isostatic rebound; Late Quaternary; Paleo topographic model

Indexed keywords

APPROXIMATION THEORY; COASTAL ZONES; DATABASE SYSTEMS; GEOGRAPHIC INFORMATION SYSTEMS; HYDROLOGY; IMAGE RECONSTRUCTION; LANDFORMS; MAPS;

LANDSCAPES;

GEOLOGY;

GIS; GLACIAL LANDFORM; LANDSCAPE CHANGE; PALEOTOPOGRAPHY; QUATERNARY; RECONSTRUCTION;

EID: 0036606812     PISSN: 00983004     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0098-3004(01)00097-8     Document Type: Article

References (46)

1. Pattern of coastal uplift and deglacierization, West Baffin Island, N.W.T
2. Postglacial emergence and submergence
3. Comparison of elevations of archaeological sites and calculated sea levels in Arctic Canada
4. Studies of glacial history in Arctic Canada. I. Pumice, radiocarbon dates, and differential postglacial uplift in the eastern Queen Elizabeth Islands
5. Radiocarbon isochrones on the disintegration of the Laurentide ice sheet
6. Greenland's rapid postglacial emergence: A result of ice-water gravitational attraction
7. Global changes in postglacial sea level: A numerical calculation
8. Deglacial chronology and uplift history: Northeastern sector
9. Quaternary geology of Boothia Peninsula and Northern district of Keewatin, Central Canadian Arctic
10. A reinterpretation of glacial and marine limits around the Northwestern Laurentide ice sheet
11. Last glacial maximum and deglaciation of Devon Island, arctic Canada: Support for an innuitian ice sheet
12. Marine molluses as indicators of environmental change in glaciated North America and Greenland during the last 18,000 years
13. Configuration and dynamics of the Laurentide ice sheet during the late Wisconsinan maximum
14. Changes in driftwood delivery to the Canadian Arctic Archipelago: The hypothesis of postglacial oscillations of the transpolar drift
15. A history of sea ice in the Canadian Arctic Archipelago based on postglacial remains of the bowhead whale (Balaena mysticetus)
16. Postglacial tectonic and sea level history of the Central Canadian Arctic
17. Paleogeography of Northern North America, 18 000-5000 years ago
18. Support for the Innuitian ice sheet in the Canadian high arctic during the last glacial maximum
19. Coalescent greenland and innuitian ice during the last glacial maximum: Revising the quaternary of the Canadian high arctic
20. On postglacial sea level
21. The paleo-great Lakes, their areas and volumes from digital elevation model studies
22. Development and assessment of the Global Land One-km Base Elevation Digital Elevation Model (GLOBE)
23. Quaternary geology of central Melville Island, Northwest Territories
24. Glacial Lake Agassiz with special reference to the mode of deformation of the beaches
25. Shoreline reconstructions for the Persian Gulf since the last glacial maximum
26. 14Cyr BP
27. Evaluating glacio-isostatic uplift from tilted shoreline data to reconstruct the paleo-bathymetry and topography of the great lakes basin
28. Calculating the volume and heat budget of glacial Lake Agassiz
29. The volume and paleobathymetry of glacial Lake Agassiz
30. The climate of the Canadian Arctic Islands and adjacent waters
31. Late Wisconsin ice sheets in North America
32. Trend surface mapping of raised shorelines
33. ETOPO 5 database, data announcement 88-MGG-02
34. The impulse response of a Maxwell Earth
35. The LAGEOS constraint on deep mantle viscosity; results from a new normal mode method for the inversion of viscoelastic relaxation spectra
36. Glacial-isostatic adjustment - I. The forward problem
37. The triangulated irregular network
38. Isobases for the Main Perth raised shoreline in South-East Scotland as determined by trend-surface analysis
39. Isostatic response to loading of the crust in Canada
40. Late quaternary vertical movements in Eastern North America: Quantitative evidence of glacio-isostatic rebound
41. A paleolimnological constraint to the extent of the last glaciation on Northern Devon Island, Canadian High Arctic