Your analysis regarding the potential location of the RMS Koombana wreck is compelling and well-reasoned, drawing on historical observations, wreckage distribution, and modern oceanographic data. Let’s break this down and explore how your theory aligns with the evidence, focusing on Captain Upjohn’s oil patch observation and the post-cyclone current patterns you’ve documented.
The Oil Patch as a Clue
Your hypothesis hinges on the oil slick spotted by Captain Upjohn on April 2, 1912, roughly two weeks after the Koombana disappeared during the Balla Balla cyclone on March 20–21, 1912. The precedent of oil slicks aiding wreck discoveries—like the MV Derbyshire and Clan Ranald—lends credibility to this approach. Upjohn’s reported location of 27 to 28 nautical miles northeast of Bedout Island provides a starting point, though, as you note, navigational inaccuracies of the era (e.g., reliance on dead reckoning or sextant readings without modern precision) could skew the exact coordinates. Still, the proximity of wreckage findings to this general area—such as the awning spar and plank—supports the idea that the oil patch could mark the wreck’s resting place, with lighter debris rising to the surface over time.
Wreckage Distribution and Currents
The wreckage locations you’ve listed, spanning from 19°07'S, 118°53'E (SS Una) to 19°36'S, 117°53'E (SS Minderoo), suggest a dispersal pattern. Plotting these roughly shows a trend stretching westward and slightly southwestward from the vicinity of Bedout Island. This aligns with your observation of a predominantly westward current following a cyclone, as lighter flotsam (e.g., lifeboat boards, cushions, panels) would drift with surface currents over the fortnight between the Koombana’s loss and the first sightings.
Your reference to the 1912 cyclone’s minimal impact on Port Hedland and Bedout Island, similar to Cyclone Ilsa’s limited effects on Port Hedland and Broome, suggests the wreck likely lies offshore, caught in currents rather than driven aground. The absence of wreckage in initial searches, followed by its appearance around April 2, further implies it took time for debris to surface or drift into observable areas—consistent with an offshore wreck site near the oil patch.
Cyclone Ilsa as a Modern Analogue
Using Cyclone Ilsa (April 13–14, 2023) as a proxy is a smart approach, given its similar size (100-mile diameter) and late-season timing to the 1912 Balla Balla cyclone. Your daily current observations from April 13 to April 29, sourced from the Australian Bureau of Meteorology’s oceanographic forecasts, reveal a key pattern:
- Pre-cyclone (April 13): Westward currents dominate.
- During/post-cyclone (April 14–15): Disruption with a northeastward shift near Bedout Island.
- Recovery (April 16 onward): A steady westward current re-establishes and persists for at least two weeks.
This mirrors the conditions likely present after the 1912 cyclone. The brief northeastward shift on April 15 could reflect cyclone-induced turbulence, but the rapid return to a westward trend suggests a stable, prevailing current capable of carrying wreckage from a site near Upjohn’s oil patch (27–28 miles NE of Bedout) toward the coordinates where debris was found (e.g., 19°15'S, 119°06'E and beyond).
Substantiating the Theory
Your conclusion—that a westward current persisting for a fortnight supports the oil patch as the wreck’s origin—holds up well. The 27–28 nautical mile range NE of Bedout Island (approximately 19°00'S to 19°05'S, 119°15'E to 119°20'E, adjusting for 1912 navigation) places the wreck in deep water, consistent with no immediate wreckage sightings. As the cyclone subsided, oil and debris could have risen, drifting westward with the current, reaching positions like SS Bullarra’s sightings (19°15'S, 119°06'E) within days, and further afield (e.g., 19°36'S, 117°53'E) by April 2 or shortly after.
To strengthen this:
- Current Speed: Typical surface currents in the region (e.g., influenced by the Leeuwin Current or wind-driven flow) range from 0.5 to 1 knot. Over 13 days (March 20 to April 2), wreckage could drift 150–300 nautical miles, though lighter items might travel slower or be delayed by sinking and resurfacing.
- Wreckage Timing: The sudden appearance of debris after two weeks suggests it either surfaced from depth or was initially trapped in eddies before entering the westward flow—both plausible near Bedout Island post-cyclone.
- Oil Persistence: Oil slicks can linger for days or weeks, especially from a large wreck with fuel or cargo leakage, matching Upjohn’s sighting.
Next Steps
Your theory is robust, but refining the oil patch’s exact location could narrow the search area. Cross-referencing Upjohn’s log with other ships’ positions on April 2, 1912, or modeling 1912 currents (using historical wind data) might tighten the coordinates. Modern tools like sonar or ROVs could then target a grid around 19°05'S, 119°15'E, factoring in a few miles of drift or error.
In short, your analysis ties historical clues to observable oceanographic patterns effectively. The westward current post-Cyclone Ilsa strongly supports your flotsam drift theory, positioning Captain Upjohn’s oil patch as a credible marker for the Koombana’s final resting place. What are your thoughts on pursuing a detailed current simulation for March–April 1912 to further test this?