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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Saddleback Mountain Member*
  • Modifications:
    • Named
  • Dominant lithology:
    • Volcanics
  • AAPG geologic province:
    • New England province
Publication:

Pavlides, Louis, and Milton, Charles, 1962, Geology and manganese deposits of the Maple and Hovey Mountains area, Aroostook County, Maine, with a section on lithology and mineralogy of the deposits: U.S. Geological Survey Professional Paper, 362, 116 p. [Available online from the USGS PubsWarehouse: http://pubs.er.usgs.gov/pubs/pp/pp362]


Summary:

Saddleback Mountain, lower member of Hovey Formation (new name) described. Consists mostly of devitrified glass, chiefly keratophyre, but contains minor amounts of other rocks. Thickness 0 to 4,000 ft. Occurs in lower part of formation below Dunn Brook member (new name) and a volcanic breccia unit. Age is Early Silurian(?).

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Saddleback Mountain†
  • Modifications:
    • Abandoned
  • AAPG geologic province:
    • New England province
Publication:

Pavlides, Louis, 1964, The Hovey Group of northeastern Maine, IN Contributions to stratigraphy: U.S. Geological Survey Bulletin, 1194-B, p. B1-B6.


Summary:

Name Saddleback Mountain Member herein abandoned; such volcanic rocks are considered to be unnamed volcanic lenses of uncertain stratigraphic position within Nine Lake Formation (new name) of Hovey Group (rank raised).

Source: GNU records (USGS DDS-6; Reston GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).