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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #122279:

Are soil tongues in northeastern Indiana periglacial relics or active fingering zones? / Kenneth M. Hinkel.

Title: Are soil tongues in northeastern Indiana periglacial relics or active fingering zones? / Kenneth M. Hinkel.
Author(s): Hinkel, Kenneth M.
Date: 1993.
In: Quaternary Research. (1993.), Vol. 39(1) (1993)
Abstract: Numerous soil tongues (or fingers) are exposed at this site, along walls of active gravel pit. Site is considered unusual both for these well-developed tongues and for apparent regularity of spacing. Tongues define sharp illuviation front which has overall appearance of high-amplitude high-frequency sinusoidal wave train. Apparent regularity of wavelength and amplitude implies some causative process which operates at same scale: discusses two such mechanisms, periglacial activity and wetting front instability.
Notes:

Quaternary Research. Vol. 39(1) :75-83 (1993).

Keywords: 551.34 -- Geocryology. Frozen ground.
551.343 -- Periglacial processes. Thermokarst.
E9 -- Glaciology: meteorology and climatology.
(73) -- United States.
(77) -- North central states.
SPRI record no.: 122279

MARCXML

LDR 01373naa#a2200000#a#4500
001 SPRI-122279
005 20240418191042.0
007 ta
008 240418s1993####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-122279
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aHinkel, Kenneth M.
245 10 ‡aAre soil tongues in northeastern Indiana periglacial relics or active fingering zones? /‡cKenneth M. Hinkel.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 75-83 :‡bill., diags., table, maps.
500 ## ‡aQuaternary Research. Vol. 39(1) :75-83 (1993).
520 3# ‡aNumerous soil tongues (or fingers) are exposed at this site, along walls of active gravel pit. Site is considered unusual both for these well-developed tongues and for apparent regularity of spacing. Tongues define sharp illuviation front which has overall appearance of high-amplitude high-frequency sinusoidal wave train. Apparent regularity of wavelength and amplitude implies some causative process which operates at same scale: discusses two such mechanisms, periglacial activity and wetting front instability.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(73) -- United States.‡2udc
651 #7 ‡a(77) -- North central states.‡2udc
773 0# ‡7nnas ‡tQuaternary Research. ‡gVol. 39(1) (1993) ‡wSPRI-46567
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240418