West Castleton

Vermont's ghost towns are marble and granite quarries and hill farms the westward migration emptied.

The West Castleton Formation is a geologic formation in New York and Vermont. It preserves fossils dating back to the Cambrian period. It is described in Vermont as "Gray silicious to black, graphitic, pyritiferous slate and phyllite, locally with interbedded thin dark grey dolostone and grey quartzite and arkosic layers. Thin, white sandy laminae commonly found in the graphitic beds."

The on-the-ground condition of West Castleton is unverified — it's listed here with unknown status. That could mean standing buildings, or an empty field. Go prepared for either, and consider sharing what you find so the record improves.

Nobody has confirmed the access situation, so treat any visit as reconnaissance: verify land ownership first, and be ready to admire from the road.

Here's the honest truth: access to West Castleton is unverified. We couldn't confirm whether the site sits on public land, private property, or something in between — so verify land ownership and local rules before visiting, and respect private property at all times. The mapped point for West Castleton is roughly 43.6591, -73.2321 — use it as a starting point and cross-reference a current topographic map before leaving pavement.

Ghost-town etiquette is simple: take only photographs. Removing artifacts is illegal on public lands and disrespectful everywhere else — and on federal land it can be a serious offense.