Chamberlain's Brook Formation Explained

Chamberlain's Brook Formation
Type:Formation
Age:Middle Cambrian
~
Period:Cambrian
Prilithology:Green, purple and red siliciclastic marine mudstones[1]
Region:Atlantic coast
Country:
Unitof:Adeyton Group[2]
Subunits:Fossil Brook Member (and others)
Underlies:Manuels River Formation (unconformably?)
Thickness:up to 14m (46feet)
Map:Chamberlains Brook Formation map.svg

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.[1] It preserves fossils, including trilobites, dating back to the lower mid-Cambrian period.[1] Its lowermost member is the Braintree Member (lowest Middle Cambrian) and the uppermost member is the Fossil Brook Member.[1]

See also

References

Notes and References

  1. 10.1666/0022-3360(2002)076<0822:MCASCA>2.0.CO;2. 2002. 76. 5. 822. Middle Cambrian (Acadian Series) Conocoryphid and Paradoxidid Trilobites from the Upper Chamberlain's Brook Formation, Newfoundland and New Brunswick. Journal of Paleontology. Kim. Dong HEE. Westrop. Stephen R.. Landing. ED.
  2. Book: Bedrock Geology of the Cap St. Mary's Peninsula. Southwest Avalon Peninsula, Newfoundland. Terrence Patrick Fletcher. 2006. Department of Natural Resources Geological Survey Newfoundland Labrador. St. John's Newfoundland. 1-55146-031-9.
  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.