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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 |
LDR 01373naa#a2200000#a#4500 001 SPRI-122279 005 20231130140751.0 007 ta 008 231130s1993####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# ‡a20231130