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Geologic Unit: Bonanza
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  • Usage in publication:
    • Bonanza Orthogneiss
  • Modifications:
    • Areal extent
  • Dominant lithology:
    • Gneiss
  • AAPG geologic province:
    • Cascades province
Publication:

Adams, J.B., 1964, Origin of the Black Peak Quartz Diorite, Northern Cascades, Washington: American Journal of Science, v. 262, no. 3, p. 290-306.


Summary:

Pg. 292 (footnote). Skagit Gneiss (Misch, 1952) has been restricted by Misch (ms) to include gneisses that can be demonstrated to be products of migmatization of sedimentary-volcanic sequence, and gneisses of doubtful origin. All the gneisses that can be shown to be derived from plutonic rocks are now separated from Skagit Gneiss (restricted). They include: Eldorado Orthogneiss, Gabriel Peak Orthogneiss, Bonanza Orthogneiss. [Age not stated by author.]
[Probably named from Bonanza Peak, northern Chelan Co., north-central WA.]

Source: US geologic names lexicon (USGS Bull. 1350, p. 82); GNU records (USGS DDS-6; Menlo 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 ([ ]).