| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.949443 |
| 003 | CaOODSP |
| 005 | 20250822114255 |
| 006 | m o d f |
| 007 | cr cn |||||||| |
| 008 | 250324t20252025nscab ob f000 0 eng d |
| 020 | |a9780660766133 |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-nf |
| 086 | 1 |aM41-11/173-2025E-PDF |
| 100 | 1 |aCameron, Gordon, |d1955- |eauthor. |
| 245 | 10|aSeabed evidence for a south-flowing ice shelf along the Newfoundland and Labrador margin / |cG.D.M. Cameron and E.L. King. |
| 264 | 1|aDartmouth, Nova Scotia : |bGeological Survey of Canada, |c2025. |
| 264 | 4|c©2025 |
| 300 | |a1 online resource (1 poster) : |billustrations, maps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aScientific presentation ; |v173 |
| 500 | |aCaption title. |
| 500 | |a"Presented to GSC Directors and the British Geological Survey at GSC-Atlantic. Date presented: March 2024." |
| 504 | |aIncludes bibliographical references. |
| 520 | |a"A new concept in the marine glacial regime has emerged from recent regional surficial geological mapping. Higher-resolution bathymetric images reveal north-south-oriented erosive lineations and shelf edge moraine, both of which are strong evidence of the presence of an ice shelf along the Newfoundland and Labrador continental margin"--Summary, page [1]. |
| 650 | 0|aIce shelves|zNewfoundland and Labrador. |
| 650 | 0|aOcean bottom|zNewfoundland and Labrador. |
| 650 | 6|aPlateformes de glace|zTerre-Neuve-et-Labrador. |
| 650 | 6|aFonds marins|zTerre-Neuve-et-Labrador. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aScientific presentation (Geological Survey of Canada)|v173.|w(CaOODSP)9.820265 |
| 856 | 40|qPDF|s20.6 MB|uhttps://publications.gc.ca/collections/collection_2025/rncan-nrcan/m41-11/M41-11-173-2025-eng.pdf |
| 856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/pb50m3jvpq |