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Geologic Unit: Garda
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Map showing publication footprint
  • Usage in publication:
    • Garda Stade*
  • Modifications:
    • Named
  • AAPG geologic province:
    • Puget Sound province
Publication:

Crandell, D.R., and Miller, R.D., 1964, Post-hypsithermal glacier advances at Mount Rainier, Washington, IN Geological Survey Research 1964: U.S. Geological Survey Professional Paper, 501-D, p. D110-D114.


Summary:

Is younger of two stades in Winthrop Creek Glaciation, northern side of Mount Rainier, Pierce Co, WA. Type section is in lateral and terminal moraines near Garda Falls. Garda Stade may have begun some time in late 12th or early 13th century. Episode of glacier expansion culminated in various valleys at different times ranging from middle of 14th to middle of 19th century. Moraines of Garda age differentiated from those of Burroughs Mountain Stade (new) age by absence of pumice layer C. Age is Recent [Holocene]

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


Map showing publication footprint
  • Usage in publication:
    • Garda Drift*
  • Modifications:
    • Overview
    • Redescribed
  • AAPG geologic province:
    • Puget Sound province
Publication:

Crandell, D.R., and Miller, R.D., 1974, Quaternary stratigraphy and extent of glaciation in the Mount Rainier region, Washington: U.S. Geological Survey Professional Paper, 847, 59 p.


Summary:

Detailed description and age of moraines of Garda and Burroughs Mountain Drifts included in report.

Source: 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 ([ ]).