| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.877742 |
| 003 | CaOODSP |
| 005 | 20241203113651 |
| 006 | m o d f |
| 007 | cr ||||||||||| |
| 008 | 190809e197604##bccbd otb f00| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |ar------ |
| 086 | 1 |aEn3-6/22E-PDF |
| 100 | 1 |aHunter, J. A. M., |eauthor. |
| 245 | 14|aThe occurrence of permafrost and frozen sub-seabottom materials in the southern Beaufort Sea / |cJ.A.M. Hunter [and five others]. |
| 246 | 34|aPermafrost and frozen sub-seabottom materials in the southern Beaufort Sea |
| 264 | 1|aVictoria, B.C. : |bBeaufort Sea Project, Dept. of the Environment, |cApril, 1976. |
| 300 | |a1 online resource (iv, 152 pages) : |bmaps, charts. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aBeaufort Sea technical report ; |v#22 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 504 | |aIncludes bibliographical references (pages 81-88). |
| 520 | |a"Permafrost conditions exist beneath most of the Beaufort Sea shelf area. As a result of large changes in the surface thermal regime in the recent geological past, non-equilibrium conditions are probably found in most areas; hence permafrost is both aggrading and degrading"--Summary. |
| 692 | 07|2gccst|aPermafrost |
| 692 | 07|2gccst|aOcean floor |
| 710 | 1 |aCanada. |bEnvironment Canada. |
| 710 | 2 |aBeaufort Sea Project (Canada) |
| 830 | #0|aBeaufort Sea technical report ;|v#22.|w(CaOODSP)9.867527 |
| 856 | 40|qPDF|s29.90 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/En3-6-22-eng.pdf |