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The Pavy
Formation is interpreted to be fluvial in origin. Trough-crossbedded sandstone facies dominate this formation and were probably channel deposits of a braided river system, with interbeds of siltstone and mudrock representing floodplain deposits. Where thicker intervals of mudrock occur,
315:
backswamp ponds or shallow-lake conditions were probably present. Only at
Watercourse Valley and Pavy River did conditions stabilize long enough for swamps to develop, producing thick coal beds.
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Heer, O (1878), "Die
Miocene Flora des Grinnell-Landes gegründet auf die von Capitan H.E. Feilden und Dr. E. Moss in der Nähe des Kap Murchison gesammelten fossilen Pflanzen",
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Flora
Fossilis Arctica: Die Fossile Flora der Polarländer
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List of fossiliferous stratigraphic units in
Nunavut
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392:Paleocene Series of North America
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115:Approximate paleocoordinates
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259:Pavy Formation (Nunavut)
422:Paleontology in Nunavut
231:Pavy Formation (Canada)
292:Carabites feildenianus
295:, dating back to the
402:Siltstone formations
262:Show map of Nunavut
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25:Stratigraphic range
330:Margaret Formation
279:geologic formation
234:Show map of Canada
387:Paleogene Nunavut
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275:Pavy Formation
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19:Pavy Formation
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137:74.3°N 13.3°W
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98:81.7°N 64.4°W
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358:Bibliography
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195:Type section
310:Description
289:insects of
142:74.3; -13.3
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103:81.7; -64.4
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76:Coordinates
381:Categories
350:Heer, 1878
338:References
204:Pavy River
301:Paleocene
297:Thanetian
200:Named for
54:Siltstone
45:Lithology
39:Formation
29:Thanetian
319:See also
70:Location
283:Nunavut
167:Country
161:Nunavut
128:13°18′W
125:74°18′N
89:64°24′W
86:81°42′N
50:Primary
372:: 1–38
304:period
287:fossil
185:Extent
179:Canada
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153:Region
277:is a
60:Other
273:The
64:Coal
35:Type
281:in
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27::
370:5
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