From Wikipedia, the free encyclopedia
Bull Arm Formation

Stratigraphic range: Ediacaran
Type Formation
Unit of Musgravetown Group
Underlies Big Head Formation, Rocky Harbour Formation [1]
Overlies Cannings Cove Formation [2]
Lithology
PrimaryVolcanics
Location
Region  Newfoundland
Country  Canada

Occurrence of the Bull Arm Formation in southeastern Newfoundland

The Bull Arm Formation is a volcanic formation cropping out in Newfoundland, the youngest of the Musgravetown Group. [3] It is defined as everything between the first and last volcanic horizon, with a recognition that some sandstones will be interbedded, and its start and finish may vary across the region depending on how widespread volcanic horizons are in practice. [4]

References

  1. ^ Normore, L.S. (2012). Geology of the Random Island map area (NTS 2C/04), Newfoundland. Curr. Res. Newfoundl. Labrador Dep. Nat. Resour. Geol. Surv. Report 12-, 121–145.
  2. ^ Normore, L.S. (2012). Geology of the Random Island map area (NTS 2C/04), Newfoundland. Curr. Res. Newfoundl. Labrador Dep. Nat. Resour. Geol. Surv. Report 12-, 121–145.
  3. ^ Normore, L.S. (2012). Geology of the Random Island map area (NTS 2C/04), Newfoundland. Curr. Res. Newfoundl. Labrador Dep. Nat. Resour. Geol. Surv. Report 12-, 121–145.
  4. ^ Fletcher, T. P. (2006). "Bedrock geology of the Cape St. Mary's Peninsula, southwest Avalon Peninsula, Newfoundland" (PDF): 117. {{ cite journal}}: Cite journal requires |journal= ( help)


From Wikipedia, the free encyclopedia
Bull Arm Formation

Stratigraphic range: Ediacaran
Type Formation
Unit of Musgravetown Group
Underlies Big Head Formation, Rocky Harbour Formation [1]
Overlies Cannings Cove Formation [2]
Lithology
PrimaryVolcanics
Location
Region  Newfoundland
Country  Canada

Occurrence of the Bull Arm Formation in southeastern Newfoundland

The Bull Arm Formation is a volcanic formation cropping out in Newfoundland, the youngest of the Musgravetown Group. [3] It is defined as everything between the first and last volcanic horizon, with a recognition that some sandstones will be interbedded, and its start and finish may vary across the region depending on how widespread volcanic horizons are in practice. [4]

References

  1. ^ Normore, L.S. (2012). Geology of the Random Island map area (NTS 2C/04), Newfoundland. Curr. Res. Newfoundl. Labrador Dep. Nat. Resour. Geol. Surv. Report 12-, 121–145.
  2. ^ Normore, L.S. (2012). Geology of the Random Island map area (NTS 2C/04), Newfoundland. Curr. Res. Newfoundl. Labrador Dep. Nat. Resour. Geol. Surv. Report 12-, 121–145.
  3. ^ Normore, L.S. (2012). Geology of the Random Island map area (NTS 2C/04), Newfoundland. Curr. Res. Newfoundl. Labrador Dep. Nat. Resour. Geol. Surv. Report 12-, 121–145.
  4. ^ Fletcher, T. P. (2006). "Bedrock geology of the Cape St. Mary's Peninsula, southwest Avalon Peninsula, Newfoundland" (PDF): 117. {{ cite journal}}: Cite journal requires |journal= ( help)



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