| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.878210 |
| 003 | CaOODSP |
| 005 | 20241203113651 |
| 006 | m o d f |
| 007 | cr ||||||||||| |
| 008 | 190819e197512##bccb otb f00| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |ar------ |
| 086 | 1 |aEn3-6/37E-PDF |
| 100 | 1 |aCooper, P. F., |cJr. |q(Paul Fenimore), |d1930-1988 |eauthor. |
| 245 | 10|aMovement and deformation of the landfast ice of the southern Beaufort Sea / |cP.F. Cooper, Jr.. |
| 264 | 1|aVictoria, B.C. : |bBeaufort Sea Project, Dept. of the Environment, |cDecember 1975. |
| 300 | |a1 online resource (16 pages) : |bmaps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aBeaufort Sea technical report ; |v#37 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 504 | |aIncludes bibliographical references (page 12). |
| 520 | |a"Every year extensive landfast ice develops along the southern coast of the Beaufort Sea. This formation is considerably more stable north and east of the Mackenzie River Delta and southeast of Herschel Island than it is in between these two areas. Yet even in these apparently stable regions observations indicate that the ice surface moves a considerable distance during a typical winter"--Summary. |
| 692 | 07|2gccst|aIce |
| 692 | 07|2gccst|aEnvironmental impact |
| 710 | 1 |aCanada. |bEnvironment Canada. |
| 710 | 2 |aBeaufort Sea Project (Canada) |
| 830 | #0|aBeaufort Sea technical report ;|v#37.|w(CaOODSP)9.867527 |
| 856 | 40|qPDF|s3.94 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/En3-6-37-eng.pdf |