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National Geologic Map Database
Geologic Unit: Sycamore Creek
Map showing publication footprint
  • Usage in publication:
    • Sycamore Creek sandstone
  • Modifications:
    • Original reference
  • AAPG geologic province:
    • Basin-and-Range province
Publication:

Lausen, Carl, and Wilson, E.D., 1925, Gold and copper deposits near Payson, Arizona: Arizona Bureau of Mines Bulletin, v. 120, no. 10, 44 p.


Summary:

Pg. 7, 12-13. Sycamore Creek sandstone. Name proposed by A.A. Stoyanow in unpublished manuscript. The formation is generally dull reddish brown in color, although some buff-colored beds are present. Is made up of a coarse quartz sand cemented chiefly by oxides of iron and carbonate of lime. Cross-bedding is locally common, and then the stratification is not well defined. Traversed by numerous joints. Pebbly layers common. Is conformably overlain by thin-bedded flaggy limestones containing fossils identified by Stoyanow as Upper Devonian. Occurs as isolated remnants south and southeast of Payson, while to north is a large area partly overlain by Redwall limestone. Upper part has been largely removed by erosion, and where overlain by Redwall limestone [Mississippian] the thickness is seldom over 150 feet. Contains fossil fishes identified by Stoyanow as undoubtably Upper Devonian. Rests unconformably on pre-Cambrian diorite and in places on older rocks. On recent map of Arizona is classified as Tapeats sandstone (Upper Cambrian). Age is Late Devonian.

Source: US geologic names lexicon (USGS Bull. 896, p. 2102).


Map showing publication footprint
  • Usage in publication:
    • Sycamore Creek formation
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Basin-and-Range province
Publication:

Stoyanow, A.A., 1926, Notes on recent stratigraphic work in Arizona: American Journal of Science, 5th series, v. 12, p. 311-324.


Summary:

Pg. 311-315. Sycamore Creek formation. Three cliff-forming sandstones, separated by beds of reddish mottled sandstone, pink-white quartzitic sandstone, and compact pink sandstone; some beds of gray limestone. Thickness 125 to 324 feet. Best exposed at Sycamore Creek, a tributary of East Verde River. Overlian by Devonian limestone. Rests on granite. Age is Devonian.

Source: US geologic names lexicon (USGS Bull. 896, p. 2102).


Map showing publication footprint
  • Usage in publication:
    • Sycamore sandstone member
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Basin-and-Range province
Publication:

Wilmarth, M.G., 1936, [Selected Geologic Names Committee remarks (ca. 1910-1937) on Cenozoic rocks and sediment of the western U.S.], IN Wilmarth, M.G., 1938, Lexicon of geologic names of the United States (including Alaska): U.S. Geological Survey Bulletin, 896, pts. 1-2, 2396 p.


Summary:

In 1936 Stoyanow gave further description of this unit and changed its name to Sycamore sandstone member of Jerome formation, as explained under 1936 entry of Jerome formation. [See Jerome.]

Source: US geologic names lexicon (USGS Bull. 896, p. 2102).


Map showing publication footprint
  • Usage in publication:
    • Sycamore sandstone
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Basin-and-Range province
Publication:

Keyes, C.R., 1942, Revision of Devonic stratigraphy of Arizona: Pan-American Geologist, v. 77, no. 3, p. 225-228.


Summary:

Pg. 228. Sycamore sandstone designated the middle part of the Jeromian series (new). Underlies East Verde limestone (new); overlies Vecol limestone (new). Thickness 75 feet. Age is Late Devonian.

Source: US geologic names lexicon (USGS Bull. 1200, p. 3797).


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 ([ ]).