19/07/2026
I've walked in to Windin Falls before, the way most people do — through the rainforest to that lookout at the edge, where the ground just stops and the valley opens up in front of you. Years ago I also flew past it in a light aircraft, camera out the window, and came away with a handful of frames looking up the valley at the falls from a distance. They sat in a folder and stayed there.
Going back through those old shots recently, something in the rock face caught my eye — diagonal fracture lines in the rock. That was reason enough to go back with the drone and get close. Today I did.
This story is told on the country of the Dulabed and Malanbarra Yidinji people, whose native title covers the upper Mulgrave catchment where Windin Creek makes its drop, and of the Ngadjon-jii, whose country lies across the neighbouring tableland to the west.
Windin Creek runs unhurried through rainforest on the Atherton Tablelands, the kind of stream you could wade across without much thought. Then the forest floor simply stops. The Great Escarpment marks the point where the tableland breaks away toward the coast, and Windin Creek meets that break head-on, dropping in a single unbroken column into the gorge that feeds the Mulgrave Valley far below. There is no rapids, no staged descent — just still water, then a hundred and more metres of air.
What the drone exposes here is the escarpment's own construction. This landscape began taking shape around a hundred million years ago, when the eastern edge of the Australian continent rifted and fell away, leaving the tableland standing high while the coastal strip sank and eroded back beneath it. Everything since has been slow retreat — rain, gravity and gullies eating westward into that uplifted edge.
The rock the creek is cutting through is older still. Mapping shows this cliff as Hodgkinson Formation — dark, thin-bedded mudstone with subordinate sandstone, minor chert and basalt, laid down as marine sediment during the Devonian, somewhere between 420 and 360 million years ago. Long after burial, the same forces that raised this coastline folded and faulted the sequence, tilting the bedding onto its edge. That's the diagonal fracture lines visible in the rock face beside the main drop — not decoration, but the old seafloor standing on end.
A few kilometres east, Mt Bartle Frere and the Bellenden Ker Range rise as granite, intruded into country like this one long after the Hodgkinson sediments had already been folded and lithified. Windin sits outside that intrusion, in the older basement rock the granite pushed into — a waterfall that has, quite by accident, cut a clean cross-section through hundreds million years of seafloor history and visible to a drone.
Video in the following post
Cheers K.