skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #119700:

The nature and geomorphological relationships of earth hummocks (thufa) in Iceland / John Gerrard.

Title: The nature and geomorphological relationships of earth hummocks (thufa) in Iceland / John Gerrard.
Author(s): Gerrard, John.
Date: 1992.
Abstract: Thufa are classified as special non-sorted forms of patterned ground, and are result of ice action in soil, although precise mode of formation is unclear. Conclusion is that thufa form within limits determined by soil grain size, soil depth, local climate, depth of soil water table and geomorphological environment. They should be seen as part of continuum of processes acting on vegetated Icelandic slopes and not treated in isolation.
Notes:

Offprint: Zeitschrift für Geomorphologie. Supplementband. Vol. 86 :173-182.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.343.72 -- Frost mounds. Pingos.
E8 -- Glaciology: frost action and permafrost.
(*35) -- Iceland.
Location(s): SCO: SPRI-SHF: 551.33
SPRI record no.: 119700

MARCXML

LDR 01248nam#a2200000#a#4500
001 SPRI-119700
005 20240418150417.0
007 ta
008 240418s1992####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-119700
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aGerrard, John.
245 14 ‡aThe nature and geomorphological relationships of earth hummocks (thufa) in Iceland /‡cJohn Gerrard.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 173-182 :‡bdiags., tables, map.
500 ## ‡aOffprint: Zeitschrift für Geomorphologie. Supplementband. Vol. 86 :173-182.
520 3# ‡aThufa are classified as special non-sorted forms of patterned ground, and are result of ice action in soil, although precise mode of formation is unclear. Conclusion is that thufa form within limits determined by soil grain size, soil depth, local climate, depth of soil water table and geomorphological environment. They should be seen as part of continuum of processes acting on vegetated Icelandic slopes and not treated in isolation.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343.72 -- Frost mounds. Pingos.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*35) -- Iceland.‡2udc
852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h551.33‡9Create 1 item record‡0Migrate
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240418