Rock face at Andover Mine with several openings beneath the trees

Andover Mine · Sussex County, New Jersey

The Window
in the Rock

A flooded passage, a high opening in the mine face, and an old illustration that makes both worth another look.

Follow the investigation
Mines & underground history / Field narrative

01 / The return

One flooded section changed the question.

Mike Sandone had already visited Andover Mine. He had seen a flooded section in one of its adits and asked Michael Girard to return with him and bring an ROV.

That joint visit took in more than Andover. They also examined the nearby Tar Hill and Longcore workings and Sulphur Hill Mine, treating the district as a connected landscape of cuts, passages, and different kinds of ore. At Andover, the immediate task was narrower: find out where the water-filled passage went.

It was a single visit together, but it opened several lines of inquiry. The water could conceal a route through the mine. The rock face held openings at different levels. An illustration from the nineteenth century showed a busier industrial landscape in roughly the same area. Each source offered part of the picture; none by itself explained the whole arrangement.

An explorer operating an underwater ROV beside a flooded opening at Andover Mine
At the waterline. The ROV made it possible to examine the flooded drift from the accessible passage.

02 / Beneath the water

A turn in the drift.

The team followed the flooded drift with the ROV. In Michael’s reading of the route, it belonged to a drift associated with the surface cuts. It made a right-angle turn and connected with an inner adit. That connection changed the flooded section from a dead end into part of a larger working plan.

The camera also recorded timber and rock structures below the waterline. Michael suspects that some may be a form of gobbing (material placed in worked-out space) and that a former drift entrance may have been closed as access shifted. The images establish that the structures are there. Their purpose and the sequence in which they were built remain interpretations, not settled findings.

ROV frame of submerged timber and stone structures in the flooded Andover drift
Submerged timbers and stone in the drift, recorded by the ROV. The on-screen depth reads 9.98 m.
Another ROV view of upright timbers in the flooded mine
A second view of the timbered structure. Its function is still under investigation.

03 / The window

An opening above the mine face.

Elsewhere in the adits, a rising passage led to an opening high in the rock face. Michael calls it the “window.” The team examined it closely. Lower on the face, they also noted a cut or indentation and other exterior structures.

These features invite a practical question: how were people and ore moving through this part of the mine at different stages of its use? The upper opening and lower cut are visible. A precise account of what each was built for has yet to be established.

View from inside the upper mine opening toward daylight
Looking outward through the upper opening. The route to it rises within the workings.

04 / The older image

The rock face in another century.

An 1855 woodcut of Andover Iron Mine, reproduced in the 1952 New Jersey Geological Survey Bulletin 62, portrays the cuts, tracks, carts, and built structures of a working mine. It offers a rare way to compare the present face with an earlier view.

Michael sees a structure in the illustration near the area of the lower indentation, beneath the upper opening. It is a useful clue, though matching every feature in an artist’s rendering to a surviving cut in the rock requires caution. The drawing helps frame the question; it does not date or identify the present structures on its own.

1855 illustration titled Andover Iron Mine Sussex County, depicting an open cut, carts, tracks, and mine structures
Andover Iron Mine, Sussex County, in an 1855 illustration reproduced in P. K. Sims and B. F. Leonard, Geology of the Andover Mining District (New Jersey Geological Survey Bulletin 62, 1952).

05 / The district

Why these neighboring mines differed.

Andover’s history extends back before the American Revolution. The 1952 survey, drawing on William S. Bayley’s earlier history, records that Continental Congress took possession of the mine during the war to supply iron and steel. The mine was reopened in 1847 and worked into the 1860s. That documented history gives the visit its larger setting, but it does not assign a Revolutionary-era date to the particular flooded drift or window.

At Sulphur Hill, Mike and Michael found the haulage tunnel. It made the neighboring operation tangible, and raised another question: why had this mine’s fortunes differed from Andover’s? The geological survey describes different ore bodies in the district and says Sulphur Hill was apparently abandoned because its ore carried too much sulfur. Tar Hill and Longcore belonged to the wider magnetite-sulfide district; Andover was the major hematite-producing mine.

The day ended with a clearer physical route through the flooded section and a longer list of historical questions. The most honest account holds both together: what the camera recorded, what the old sources document, and what still needs to be tested against the rock.

Explorer standing in water within a passage at Sulphur Hill Mine
The haulage tunnel at Sulphur Hill Mine, explored during the same district visit.
A water-filled tunnel at Tar Hill Mine
Tar Hill, another of the neighboring workings examined on the outing.

Sources & field record

Following the evidence.

This account combines Michael Girard’s recollection of the single joint visit with Mike Sandone, supplied field photographs and ROV frames, and published mining history. The proposed function of the submerged structures and upper window remains open.

Beyond this mine

Where the water changes the map.

See how Michael uses underwater vehicles to explore flooded caves and abandoned workings.

Explore Beyond the Sump →
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