Zobrazeno 1 - 10
of 46
pro vyhledávání: '"C. B. Crampton"'
Autor:
C. B. Crampton
Publikováno v:
Canadian Journal of Soil Science. 59:215-219
Maps showing the distribution of soil drainage classes on Burnaby Mountain in the Greater Vancouver urban area during 1974 and 1978, and systematic profile investigations during the intervening years, have revealed distinct changes. Construction of S
Autor:
C. B. Crampton
Publikováno v:
Canadian Journal of Earth Sciences. 15:655-659
The depth of icy permafrost below the active layer in northeastern British Columbia has been mapped in subparallel north-northwest and south-southeast zones, the thickest permafrost occurring in organic terrain near the Alberta border. Across the Roc
Autor:
C. B. Crampton
Publikováno v:
Canadian Journal of Earth Sciences. 14:639-649
Microrelief consisting of mounds or hummocks was examined at selected sites in the discontinuous and continuous permafrost zones of the Canadian north. Observations of the macromorphology and micromorphology of the mounds were used to interpret the d
Autor:
C. B. Crampton, Edward C. Schneider
Publikováno v:
American Journal of Physiology-Legacy Content. 110:14-18
Autor:
C. B. Crampton
Publikováno v:
Forestry. 39:171-188
Autor:
C. B. Crampton, Edward C. Schneider
Publikováno v:
American Journal of Physiology-Legacy Content. 112:202-206
Autor:
Edward C. Schneider, C. B. Crampton
Publikováno v:
American Journal of Physiology-Legacy Content. 112:695-698
Autor:
C. B. Crampton
Publikováno v:
Grass and Forage Science. 21:70-79
The present and potential land use of rough hill pastures in Brecknockshire has been investigated. The interests of the Brecon Beacons National Park, reservoir, Forestry Commission and commonland need not compete, but could be complementary. Areas co
Autor:
C. B. Crampton
Publikováno v:
Canadian Journal of Earth Sciences. 10:432-438
Terrain types in the southern Mackenzie River valley can be arranged into morphological series which are, in part, continuous and, in part, discontinuous, so as to allow speculation on the probable evolution of organic terrain in the area from frozen
Autor:
C. B. Crampton
Publikováno v:
Geological Magazine. 94:89-103
The great majority of Moine lineations are mica structures, and together with a parallel preferred orientation of epidote [010]-axes, are directed mainly into the south-east quadrant. This orientation is retained within the crush zone alongside the M