— — the cave that closed itself.
“A small hydrothermal cave in the dry hills west of Utah Lake. Closed and sealed since November 2009, after a rescue attempt that ran twenty-six hours and ended the way it ended. The hillside above looks like any other in Juab County. A plaque marks what is below. Some places you remember by what is no longer entered.
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The cave sits in the dry foothills of the West Tintic Mountains, southwest of Utah Lake near the small town of Goshen, in Utah County. Discovered in 1960 by Dale Green, it formed through hydrothermal action rather than the slow surface dissolution of most limestone caves. Mapped passages run roughly 1,400 feet and reach about 145 feet below the surface. The land is held by the Utah School and Institutional Trust Lands Administration. The entrance was permanently sealed with concrete in November 2009.
After the rescue attempt of November 2009, the State of Utah and the Jones family agreed the cave would not reopen. The body of John Edward Jones, a twenty-six-year-old medical student from Stansbury Park, remains where he came to rest in a narrow side passage called Ed's Push. The entrance was filled, the shaft capped, and a small bronze plaque set into the stone above. The hill itself is quiet again. No visitor center, no path, no trail.
There is nothing to visit. The cave was closed by the landowner immediately after the 2009 incident, the entrance filled with concrete, and access prohibited. The plaque is the only marker. Curious hikers sometimes find the spot from a pull-off off Pole Canyon Road, then stand a moment and walk back. The Utah Office of Tourism does not list it among destinations. For those who want context, the documentary The Last Descent (2016) reconstructs the rescue more carefully than most accounts online.