Georgetown
Deposit type & geology
Silver carbonate-replacement (no gold documented).
Carbonate-hosted oxidized lead-silver-zinc suite.
Age: Regionally grouped with Laramide polymetallic replacement districts (Fierro-Hanover, Chloride Flat).
Structural geology & terrain
Vein/structure orientation: —
Named controlling structure: —
Elevation range: ~6,526 ft
Willow Creek valley, pinyon-juniper, near-abandoned.
High-resolution terrain
~6 m/pixel lidar-derived hillshade (USGS 3DEP) — fine enough to reveal old mine workings, waste-rock piles, trenches, and roads the statewide terrain layer can’t show.
Historical production
No gold commodity found listed for this district in any source consulted — included for transparency as a district that was researched and explicitly ruled out as a gold producer, not overlooked.
Sources: Mindat (secondary, flagged); USGS district classification catalog; USGS Professional Paper 610 (Koschmann & Bergendahl 1968, cross-referenced) researched — see sources
Current status
Ghost town; post office closed in the 1930s. No current activity of any kind identified.
Not a gold district
No gold commodity documented — claim-activity recency is not applicable to this entry.
Land ownership & directions
Land ownership for this district was not independently confirmed in this session's research — verify directly before relying on it.
Mixed/unclear. Grant County.
See specimen photos (mindat.org) → — this app doesn’t host specimen photos itself; this searches mindat.org’s own mineral-specimen database, which isn’t necessarily specific to this exact district.
This pin is a generalized district/historic-site reference point, not a surveyed claim boundary — routes may cross private or patented inholdings where public access isn’t guaranteed even if a road reaches the site. Backcountry mine areas commonly have unmarked shafts, unstable ground, and no cell service; confirm current access and safety conditions (land manager, county, or landowner) before heading out.
Geologist’s read
Deliberately included to show the research process's negative results, not just positive hits — a district can be geologically and historically real without being a gold play. Note: some historic USGS classifications loosely group Georgetown with the broader Santa Rita/“Central” mining complex, which does have documented byproduct gold (see the Santa Rita/Chino entry) — but no source found attributes any gold production to Georgetown's own carbonate-replacement silver deposits specifically.