Judge’s Spring | Skipper Cave

Location: Washington County, Florida, United States

Judge’s Spring, also known as Skipper Cave, is located on Holmes Creek southwest of Vernon and not far from Hidden Spring.

The spring lies at the end of a small branch in a shallow basin. Surface visibility in the basin is often limited due to tannic water, making the cave opening difficult to identify from above.

The system contains a moderately sized entrance, a small cavern zone, and multiple interior passage types with distinct characteristics.

Geological Context
Structure & Layout
Hydrological Characteristics
Exploration & Line Extensions
Cave Data
Current Status

Geological Context

Judge’s Spring discharges from Florida’s karst limestone into a small basin connected to Holmes Creek.

The basin frequently contains tannic or murky water, reducing surface visibility. An old wooden dock remains submerged near the shoreline, indicating prior surface activity at the site. The dock has several nails protruding from it, so caution should be used when in close proximity to it.

The limestone structure reflects typical Holmes Creek characteristics, with varied passage morphology and sediment-sensitive sections.

Structure & Layout

Judge’s Spring contains three distinct interior areas, each with different structural characteristics.

The main passage continues straight for several hundred feet before gradually decreasing in size farther from the entrance.

Two primary offshoot passages branch from the main line:

The first offshoot leads into a moderately sized corridor that slopes upward to approximately 10 feet of depth. Near the end of this passage, an additional continuation was identified and extended.
The second offshoot leads into a deeper, silty maze of tunnels that progressively narrow and branch.

The silty maze section is particularly sensitive to disturbance and requires careful propulsion to maintain visibility.

Hydrological Characteristics

Judge’s Spring exhibits moderate discharge typical of Holmes Creek systems.

Water clarity at the surface is often tannic and limited, though interior visibility stabilizes beyond the entrance zone.

Flow is manageable within the primary passages but may concentrate in narrower sections of the maze.

Exploration & Line Extensions

In the mid-2010s, extensions were made to both primary offshoot passages. Additional line was placed in the upward-sloping corridor beyond the previously documented terminus. Within the deeper maze section, one of the branching tunnels was extended and documented, clarifying the layout of that portion of the system. These efforts improved understanding of the cave’s internal branching complexity.

In the mid-2010s, Jason Richards surveyed and published a map of this cave.

Portions of this cave system were explored and surveyed during cave dives conducted by Rob Neto while documenting Florida’s underwater cave systems for the book The Hidden Rivers of Florida.

Cave Data

Location: Washington County, Florida
Water Source: Floridan Aquifer
Cave Type: Submerged limestone cave system
Depth Range: 10–80 feet (3–24 meters)
Water Temperature: ~68°F (20°C)
Geology: Karst limestone
Primary Access: Spring vent
Exploration Status: Partially explored

Current Status

Judge’s Spring remains a technically straightforward but sediment-sensitive system.

The combination of:

Murky surface basin
Cavern-to-restriction transition
Three distinct structural zones
Extended offshoot passages
Silty maze configuration

gives the cave three distinctly different interior environments within a relatively compact footprint.

Proper buoyancy control is necessary to maintain visibility, particularly in the deeper maze sections.

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