Giant Grooves Made by Concentrated Basal Ice Streams

Abstract Glacial grooves are known on all the flat-lying limestone islands in western Lake Erie. The largest megagroove complexes are on Kelleys Island, each 2–6 m deep, 5–20 m wide, and 100–400 m long before quarrying. Each megagroove floor is rolling with second-order rounded ridges and “sine-shap...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Goldthwait, R. P.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000029919
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029919
id crcambridgeupr:10.1017/s0022143000029919
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000029919 2024-04-07T07:53:41+00:00 Giant Grooves Made by Concentrated Basal Ice Streams Goldthwait, R. P. 1979 http://dx.doi.org/10.1017/s0022143000029919 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029919 en eng Cambridge University Press (CUP) Journal of Glaciology volume 23, issue 89, page 297-307 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000029919 2024-03-08T00:34:51Z Abstract Glacial grooves are known on all the flat-lying limestone islands in western Lake Erie. The largest megagroove complexes are on Kelleys Island, each 2–6 m deep, 5–20 m wide, and 100–400 m long before quarrying. Each megagroove floor is rolling with second-order rounded ridges and “sine-shaped” grooves 10–90 cm deep, and 5–40 m long. Furthermore, these are gouged laterally by sharply curving and nesting gouges up to 10 cm deep. All grooves exhibit third-order striation up to 1–2 mm deep and 5–200 cm long made by individual tools of debris traveling mostly 240–260°. Ice of the Erie lobe was under compressive flow as it rose from 9 m below present lake level to 12 m above. Some sort of ice vortices (fixed eddies in the basal ice stream) are postulated to make the scoop marks and ridge ends. Fast-moving ice rather than water or a slurry is favored because there are no percussion marks. Very likely, a till mat of interfering engraving points is required. A strong convergence (2× to 10×) of striae into the deepest grooves indicates squeezing together of the debris tools and increase in local ice velocity. Interglacial subareal streams may well have shaped the initial trough up which these ice streams concentrated, because dendritic tributary grooves intersect, and main groove sets curve as much as 10° or 20°. Furthermore, sharp 100–180° meander curves are preserved at the bottom of the deepest grooves. Hiram-age clay-till with rare erratics half fills the original grooves; it shows that this groove cutting was completed before 15 500 14 C years ago. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Western Lake ENVELOPE(-128.106,-128.106,52.663,52.663) Limestone Islands ENVELOPE(-131.618,-131.618,52.909,52.909) Journal of Glaciology 23 89 297 307
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Goldthwait, R. P.
Giant Grooves Made by Concentrated Basal Ice Streams
topic_facet Earth-Surface Processes
description Abstract Glacial grooves are known on all the flat-lying limestone islands in western Lake Erie. The largest megagroove complexes are on Kelleys Island, each 2–6 m deep, 5–20 m wide, and 100–400 m long before quarrying. Each megagroove floor is rolling with second-order rounded ridges and “sine-shaped” grooves 10–90 cm deep, and 5–40 m long. Furthermore, these are gouged laterally by sharply curving and nesting gouges up to 10 cm deep. All grooves exhibit third-order striation up to 1–2 mm deep and 5–200 cm long made by individual tools of debris traveling mostly 240–260°. Ice of the Erie lobe was under compressive flow as it rose from 9 m below present lake level to 12 m above. Some sort of ice vortices (fixed eddies in the basal ice stream) are postulated to make the scoop marks and ridge ends. Fast-moving ice rather than water or a slurry is favored because there are no percussion marks. Very likely, a till mat of interfering engraving points is required. A strong convergence (2× to 10×) of striae into the deepest grooves indicates squeezing together of the debris tools and increase in local ice velocity. Interglacial subareal streams may well have shaped the initial trough up which these ice streams concentrated, because dendritic tributary grooves intersect, and main groove sets curve as much as 10° or 20°. Furthermore, sharp 100–180° meander curves are preserved at the bottom of the deepest grooves. Hiram-age clay-till with rare erratics half fills the original grooves; it shows that this groove cutting was completed before 15 500 14 C years ago.
format Article in Journal/Newspaper
author Goldthwait, R. P.
author_facet Goldthwait, R. P.
author_sort Goldthwait, R. P.
title Giant Grooves Made by Concentrated Basal Ice Streams
title_short Giant Grooves Made by Concentrated Basal Ice Streams
title_full Giant Grooves Made by Concentrated Basal Ice Streams
title_fullStr Giant Grooves Made by Concentrated Basal Ice Streams
title_full_unstemmed Giant Grooves Made by Concentrated Basal Ice Streams
title_sort giant grooves made by concentrated basal ice streams
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000029919
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029919
long_lat ENVELOPE(-128.106,-128.106,52.663,52.663)
ENVELOPE(-131.618,-131.618,52.909,52.909)
geographic Western Lake
Limestone Islands
geographic_facet Western Lake
Limestone Islands
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 23, issue 89, page 297-307
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000029919
container_title Journal of Glaciology
container_volume 23
container_issue 89
container_start_page 297
op_container_end_page 307
_version_ 1795669767745437696