Chamberlain's Brook Formation

(Redirected from Chamberlain's Brook Fm)

The Chamberlain's Brook Formation is a thin but distinctive geologic formation of dark red calcareous mudstones[3] that crops out from Rhode Island to Massachusetts and, Nova Scotia, New Brunswick and Newfoundland.[2] It preserves fossils, including trilobites, dating back to the lower mid-Cambrian period.[2] Its lowermost member is the Braintree Member (lowest Middle Cambrian) and the uppermost member is the Fossil Brook Member.[2]

Chamberlain's Brook Formation
Stratigraphic range: Middle Cambrian
~509–506 Ma
TypeFormation
Unit ofAdeyton Group[1]
Sub-unitsFossil Brook Member (and others)
UnderliesManuels River Formation (unconformably?)[2]
Thicknessup to 14 m (46 ft)[2]
Lithology
PrimaryGreen, purple and red siliciclastic marine mudstones[2]
Location
RegionAtlantic coast
Country United States
 Canada

Occurrence of the Chamberlain's Brook Formation in southeastern Newfoundland

See also

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References

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  1. ^ Terrence Patrick Fletcher (2006). Bedrock Geology of the Cap St. Mary's Peninsula. Southwest Avalon Peninsula, Newfoundland (PDF). St. John's Newfoundland: Department of Natural Resources Geological Survey Newfoundland Labrador. ISBN 1-55146-031-9.
  2. ^ a b c d e f Kim, Dong HEE; Westrop, Stephen R.; Landing, ED (2002). "Middle Cambrian (Acadian Series) Conocoryphid and Paradoxidid Trilobites from the Upper Chamberlain's Brook Formation, Newfoundland and New Brunswick". Journal of Paleontology. 76 (5): 822. doi:10.1666/0022-3360(2002)076<0822:MCASCA>2.0.CO;2.
  3. ^ Normore, L. S. 2012: GEOLOGY OF THE RANDOM ISLAND MAP AREA (Nts 2C/04), Newfoundland. Current Research (2012) Newfoundland and Labrador Department of Natural Resources Geological Survey Report 12-:121–145.