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Record #129442:
Sedimentology of Wartanian outwash near Belchatów, central Poland / Dariusz Krzyszkowski.
Title: | Sedimentology of Wartanian outwash near Belchatów, central Poland / Dariusz Krzyszkowski. |
Author(s): | Krzyszkowski, Dariusz. |
Date: | 1994. |
In: | Boreas. (1994.), Vol. 23(2) (1994) |
Abstract: | This braided outwash was formed synchronously by two river systems: glacier streams flowing from north-west and west, and periglacial rivers flowing from south and south-west. Alluvial fan formed, which later developed into aggrading fan due to rising water level on proglacial lake to north. Braided streams were represented by relatively low-energy systems with shallow-channel and/or transverse bar deposition. Sporadically, rapid inflows of meltwater caused more energetic conditions and formation of large scours. Latter were found only in glacier streams and this was confirmed by palaeocurrent measurements and analyses of quartz roundness. |
Notes: | Boreas. Vol. 23(2) :149-163 (1994). |
Keywords: | 551.33 -- Glacial geology. 551.332.58 -- Outwash plains. 551.332.24 -- Glacio-fluvial deposits. 551.3.051 -- Sedimentation and stratification. 551.1/.4 -- Geology. E7 -- Glaciology: glacial geology and ice ages. (438) -- Poland. |
SPRI record no.: | 129442 |
LDR 01542naa#a2200000#a#4500 001 SPRI-129442 005 20240418003348.0 007 ta 008 240418s1994####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-129442 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aKrzyszkowski, Dariusz. 245 10 ‡aSedimentology of Wartanian outwash near Belchatów, central Poland /‡cDariusz Krzyszkowski. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1994. 300 ## ‡ap. 149-163 :‡bill., diags., tables, maps. 500 ## ‡aBoreas. Vol. 23(2) :149-163 (1994). 520 3# ‡aThis braided outwash was formed synchronously by two river systems: glacier streams flowing from north-west and west, and periglacial rivers flowing from south and south-west. Alluvial fan formed, which later developed into aggrading fan due to rising water level on proglacial lake to north. Braided streams were represented by relatively low-energy systems with shallow-channel and/or transverse bar deposition. Sporadically, rapid inflows of meltwater caused more energetic conditions and formation of large scours. Latter were found only in glacier streams and this was confirmed by palaeocurrent measurements and analyses of quartz roundness. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.332.58 -- Outwash plains.‡2udc 650 07 ‡a551.332.24 -- Glacio-fluvial deposits.‡2udc 650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(438) -- Poland.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 23(2) (1994) ‡wSPRI-56035 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418