Geology Reference
In-Depth Information
Senneset. K., ed. (2000).
Proceedings, International Workshop on Permafrost Engineering
, Long-
yearbyen, Svalbard, Norway, 18-21 June. Norwegian University of Science and Technology
(NTNU)/The University Courses on Svalbard (UNIS), 327 pp.
Seppälä, M. (1971). Evolution of eolian relief of the Kaamasjoki-Kiell-ajoki River Basin in Finnish
Lapland.
Fennia
,
104
, 543-562.
Seppälä, M. (1972a). Location, morphology and orientation of inland dunes in Northern Sweden.
Geografi ska Annaler
,
54A
, 85-104.
Seppälä, M. (1972b). The term “palsa”:
Zeitschrift für Geomorphologie
,
16
, 463.
Seppälä, M. (1974). Some quantitative measurements of the present-day defl ation on Hietatievat,
Finnish Lapland.
Abhandlungen der Akademie der Wissenschaften Göttingen, Math.-Phys.
Klasse
, III,
29
, 208-220.
Seppälä, M. (1982). An experimental study of the formation of palsas. In: French, H. M., ed.,
Pro-
ceedings, Fourth Canadian Permafrost Conference
, Calgary, Alberta. National Research Council
of Canada, Ottawa, pp. 36-42.
Seppälä, M. (1995a). How to make a palsa: a fi eld experiment on permafrost formation.
Zeitschrift
für Geomorphologie
, suppl.
99
, 91-96.
Seppälä, M. (1995b). Defl ation and redeposition of sand dunes in Finnish Lapland.
Quaternary
Science Reviews
,
14
, 799-809.
Seppälä, M. (1997). Piping causing thermokarst in permafrost, Ungava Peninsula, Québec, Canada.
Geomorphology
,
20
, 313-319.
Seppälä, M. (1998). New permafrost formed in peat hummocks (pounus), Finnish Lapland.
Perma-
frost and Periglacial Processes
,
9
, 367-374.
Seppälä, M. (2004).
Wind as a Geomorphic Agent in Cold Climates
. Cambridge University Press,
Cambridge, 368 pp.
Seppälä, M. (2005). Frost heave on earth hummocks (pounus) in Finnish Lapland.
Norsk Geografi sk
Tidsskrift
,
59
, 171-176.
Seppälä, M., Gray, J., Richard, J., (1988). The development of depressed-centre ice-wedge polygons
in the northernmost Ungava Peninsula, Québec, Canada. In: Senneset, K., ed.,
Permafrost, Pro-
ceedings of the Fifth International Conference on Permafrost
, 2-5 August, Trondheim, Norway.
Tapir, Trondheim, vol. 1, pp. 862-866.
Serrano, E., Martinez de Pison, E., Lopez-Martinez, J. (1996). Periglacial and nival landforms and
deposits. In: Lopez-Martinez, J., Thomson, M. R. A., Thomson, J. W., eds.,
Geomorphological
Map of Byers Peninsula, Livingston Island
, BAS GEOMAP series, sheet 5-A, map (scale
1:25000) and text. British Antarctic Survey, Natural Environmental Research Council, pp.
28-34.
Shackleton, N. J., Opdyke, N. D. (1973). Oxygen isotope and palaeomagnetic stratigraphy of equato-
rial Pacifi c core V28-239: oxygen isotope temperatures and ice volumes on a 10-5 and 10-6 year
scale.
Quaternary Research
,
3
, 39-55.
Shackleton, N. J., Berger, A., Peltier, W. A. (1990). An alternative astronomical calibration of the
lower Pleistocene timescale based on ODP Site 677.
Transactions of the Royal Society of Edin-
burgh: Earth Sciences
,
81
, 251-261.
Shamanova, I. I. (1971). Manifestation of erosion in permafrost on the Yamal Peninsula.
Izvestiya
Akad. nauk SSSR
, Ser. Geograf. [News of the USSR Academy of Sciences, Geographic Series],
no. 2, 92-98 (in Russian; English translation, 1971,
Soviet Hydrology: Selected Papers
, no. 2,
198-203).
Shang, J. (1982). Some characteristics of permafrost along the Qinghai-Xizang Plateau. In:
Proceed-
ings, First Chinese Conference on Glaciology and Geocryology
. China Science Press, Beijing, pp.
38-43 (in Chinese).
Sharp, R. P. (1942a). Ground ice mounds in tundra.
Geographical Review
,
32
, 417-423.
Sharp, R. P. (1942b). Periglacial involutions in northeastern Illinois.
Journal of Geology
,
50
,
113-133.
Sharp, R. P. (1949). Pleistocene ventifacts east of the Big Horn mountains, Wyoming.
Journal of
Geology
,
57
, 175-195.
Shepherd, A., Wingham, D. J., Mansley, J. A., Corr, H. F. (2001). Inland thinning of Pine Island
Glacier, West Antarctica.
Science
,
291
, 862-864.