Bozel Spring
Location: Jackson County, Florida, United States
Bozel, also known as Baltzell Spring, is a spring system located off the Chipola River approximately 1.25 miles upstream from the Florida Caverns State Park boat launch.
The spring features four vents, three of which are accessible to divers under appropriate conditions. The system includes a prominent main vent at the end of a scenic spring run as well as additional openings located within a nearby basin surrounded by private property.
Bozel is notable for its varied passage structure, vertical entry, restrictive sections, and significant exploration extensions completed in the mid-2010s.
Geological Context
Structure & Layout
Exploration History
Hydrological Characteristics
Cave Data
Current Status
Geological Context
Bozel formed within Florida’s karst limestone and discharges into the Chipola River. The spring run flows approximately 400 feet from a basin surrounded by cypress trees and cypress knees, creating one of the more visually distinctive spring environments in the region.
The main basin is visible from an old, abandoned red cabin located on property owned by Southern Cattle Company.
Additional vents are located in a separate basin approximately thirty feet from the spring run. These openings lie within private property boundaries and require landowner permission for lawful access.
Structure & Layout
Main Vent
The primary vent is located at the end of the spring run in a large, clear basin. The underwater opening drops vertically to approximately 45 feet before transitioning into modest passage.
The first 300 feet of passage are highly variable in depth, often described as “roller coaster” in profile due to frequent depth changes.
Shortly past this fissure is a third opening. This entrance can also be reached from private property.
Approximately 100 feet beyond the fissure, the cave transforms dramatically.
Basin Vents
Two additional accessible vents are located in a basin approximately thirty feet from the spring run.
- The second opening drops vertically to approximately 15 feet before continuing into modest passage.
- After the second opening, a fissure section is encountered that is accessible only to sidemount divers.
- Just beyond the fissure lies a third opening.
The third opening has historically been accessed by backmount divers entering via private property without permission. Legal access requires landowner approval.
Interior Features
Approximately 100 feet beyond the fissure, the character of the cave changes significantly.
The passage deepens and opens into a large chamber known as the Stadium, named for its size and sloping floor profile.
The Stadium is characterized by:
- Expansive dimensions
- A sloping limestone floor
- Depth ranging from approximately 60 feet to 120 feet
The chamber represents one of the most visually distinctive features within the Chipola River spring systems.
Beyond this chamber, the cave continues in structured limestone passage.
Exploration History
In 2015, an exploration project extended the surveyed passage from 2,571 feet to 5,718 feet.
The main line was advanced more than 200 feet beyond its prior terminus. Additional adjacent sections were discovered and documented.
Two notable passage areas were identified and named:
- The Blue Room
- The Brown Room
These names reflect visual characteristics observed during exploration.
Team members involved in these exploration efforts included Rob Neto, Eric Alexander, and Mike Baker.
Bozel’s multi-vent configuration and depth transitions distinguish it from many other Chipola River systems. For a broader perspective on how Bozel fits within the larger landscape of Florida Panhandle cave systems, see the Guide to Cave Diving in the Florida Panhandle.
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.
Hydrological Characteristics
Bozel exhibits steady spring discharge influenced by Chipola River stage.
The multi-vent structure creates varied internal flow patterns depending on river conditions.
The combination of:
- Vertical drop
- Rolling shallow passage
- Fissure restriction
- Large chamber expansion
creates structural diversity within a relatively compact footprint.
Cave Data
Location: Jackson County, Florida
Water Source: Floridan Aquifer
Cave Type: Submerged limestone cave system
Depth Range: 15–120 feet (4.5–37 meters)
Water Temperature: ~68°F (20°C)
Geology: Karst limestone
Primary Access: Spring vent
Exploration Status: Fully explored
Current Status
Bozel remains an active and structurally complex spring system within the Chipola River watershed.
Access considerations include:
- River conditions
- Private property boundaries
- Variable depth profiles
- Restrictive sidemount-only sections
Bozel represents one of the more architecturally diverse spring cave systems within the Chipola River basin.
Related Systems
Maddachalk Spring
Maunds Spring
Return to Chipola River Spring Systems
Return to Florida Panhandle Cave Systems
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