Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Kamil Zaniewski"'
Publikováno v:
World Geomorphological Landscapes ISBN: 9783030351359
The scenery and landforms of the Thunder Bay region result from a varied bedrock geology, particularly notable being the flat-topped mountain features of the Sleeping Giant, Mt. McKay and others, resulting from the intrusion of the Logan diabase sill
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd9b34825f69c8571e523040cdf5e5c5
https://doi.org/10.1007/978-3-030-35137-3_6
https://doi.org/10.1007/978-3-030-35137-3_6
Autor:
Kamil Zaniewski, Philip Fralick
Publikováno v:
Sedimentology. 59:1030-1049
Descriptions of fluvial systems operating prior to significant terrestrial macrophyte vegetation have concentrated on assessing the impact of plant evolution on channel style; this is probably in part due to the scarcity of well-developed floodplain
Publikováno v:
CATENA. 63:109-127
A new method of image analysis was tested on digital micro-photographs of glacial sediments. The method incorporated multispectral image classification algorithm to identify and separate the major components of each image. The resulting ‘maps’ sh
Publikováno v:
Journal of Sedimentary Research. 74:760-769
Samples of gravity cores recovered from Yakutat Bay and Glacier Bay in southeast Alaska were examined in thin section. The samples, representing rhythmically laminated plume deposits, current-derived silts and sands, and iceberg-rafted diamicts, exhi
Autor:
Kamil Zaniewski, John Menzies
Publikováno v:
Sedimentary Geology. 157:31-48
Examination of a modern debris flow in comparison with a Quaternary diamicton from which it has been derived reveals significant differentiating sedimentological characteristics. The two sediments were examined using micromorphological analyses. Thin
Autor:
Kamil Zaniewski, Daniel P. McCarthy
Publikováno v:
Arctic, Antarctic, and Alpine Research. 33:107-113
Image analysis software was used to obtain various measures of thalli in crustose lichen communities. Lichens growing on flat-faced quartzite boulders in two glacier forefields were photographed an...
Publikováno v:
Sedimentary Geology. 111:161-175
Discussion on the process of drumlin formation has been ongoing for over a century. At present, two dominant schools of thought prevail, viz. formation by (a) subglacial hydraulic mechanisms, and (b) due to subglacial sediment deformation. The latter