2026
Trip to the Kimberley, July
Trip to the Kimberley, July
15 Day APT Kimberly Complete
Part 1
Broome/Windjana Gorge/Tunnel Creek/Fitzroy Crossing/Purnululu National Park/Bungle Bungles
Thursday, 9 July
Depart at 11:05 from Brisbane via Perth to arrive at 18:00 in Broome
4WD Tour
10 July
Broome is famous for:
...sunsets
...Boab trees
...Paspaley ...Cable Beach Resort
...the world's oldest cinema ... no traffic lights
You know you're in Broome when you keep going around in circles...
We checked into the Cable Beach Club Resort & Spa and waited for sunset.
Can't take much longer
Down further
Almost
Gone
We met our Tour Director Leigh and 22 fellow travellers over Dinner at Cable Beach Resort.
Saturday, 11 July
Departing Broome
We travelled the Great Northern Highway.
RNM checking out for roadworthiness
as are Carol and Nada
Evolution of the Kimberley Landscape
The Kimberley landscape is ancient and has been evolving for the past 250 million years. Climate and erosion by water, wind, and ice have worn away hills and valleys, leaving isolated hills. If earth movements uplift the surface, the landscape becomes rejuvenated as rivers and streams cut down into and erode the old surface, forming a new system of hills and valleys.
The following is a Sequence of Geological Events, showing the millions of years it took to form the West and East Kimberley:
Erosion produced the present landscape of hills, valleys, and gorges, driven by the uplift of the low Kimberley surface, which began 20 million years ago as Australia began to drift north towards Asia. A rise in sea level about 17,000 years ago, following the last ice age, drowned the Kimberley coastline, with the sea now filling what were once river valleys.
Today, we can marvel at the imposing sights, the famed black-and-orange-striped domes, the geological wonders, the Indigenous cultural significance and its overall magnificence.
We began our first walk to Bandilngan (Windjana Gorge), where sheer cliffs tower above glistening white sands.
Bandilngan National Park
An ancient marine fossil embedded in the gorge walls, but you've got to know where to look, Leigh knew
Tunnel Creek (Dimulurru)
Over the past 20 million years, water has carved through the limestone of the Napier Range to form this 750m-long tunnel, once part of an ocean reef system.
Dimulurru was used as a hideout by the Aboriginal resistance fighter Jandamarra of the Bunuba people, who led a 3-year campaign against British colonisation. He was killed in 1897, aged 24.
Dimalurru follows a prominent joint or fault that has acted as a channel for groundwater flowing through the limestone and eroding the tunnel.
RNM climbing
Be CROCWISE in the Kimberley... Alas, RNM saw the sign and retreated hastily
Omnipresent Boab trees
Fitzroy River Lodge pays homage to local identity Maxine McDonald, whose portrait graces the Lodge's walls.
Maxine McDonald
1914 - 2003
Maxine became famous throughout the Kimberley for bringing high culture and hospitality to the remote outback, often hosting guests, regional travellers, and visiting politicians on the wide verandahs of Fossil Downs Station, near the junction of Margaret and Fitzroy Rivers. She was educated in Sydney and worked there as a high-society fashion model until she married William 'Bill' McDonald in 1938, whose pioneering family had established Fossil Downs Station in the 1880s after a historic 3-year overland cattle drive from NSW.
This remarkable woman actively advocated for living conditions, healthcare, and education in isolated pastoral communities across northern WA. In 1981, she received an MBR for her outstanding service to the Kimberley community.
12 July
Departing Fitzroy River Lodge
We headed to Mimbi Caves, home to the Gooniyandi people and a place of spiritual significance for thousands of years.
Mueller Ranges
View of the Window - natural window in a sandstone dome
Mimbi Caves
An intricate system of high, narrow, interconnected passageways forms underground pools. Water only flows through the caves after prolonged heavy rain during the wet season. During the dry season, water dripping from the cave roof onto the floor precipitates calcite to form stalagmites, or flows down the walls to form curtains of flowstone.
Purnululu Conservation Park
Piccaninny Gorge TrekCharacterised by white sand, rounded pebbles, and some rocky sections artfully sculptured by the forces of water, Piccaninny Creek bed is an attraction in its own right. Majestic sandstone domes, orange coloured rock walls and the ever-blue Kimberley sky round off this picture-perfect scenery. The 'sculptured' creek bed of Picaninny Creek
Leigh carrying supplies for 22 travellers ...Heading towards Cathedral Gorge
A great place for reflection about life ...
Cathedral Gorge is a world-famous natural arena, equal in size to a cathedral and rivalling the acoustics of an opera house. How I would have loved to hear Renato Dolcini sing here...
Embraced by vertical, deeply undercut rock walls, the massive amphitheatre is humbling in its grandeur.
Time to leave this magical place and head towards another...Bellburn AirstripPurnululu from the air with HeliSpiritA30 Bungle Bungle Domes & Red Rock Gorges Flight over Red Rock Gorge, Piccanniny Gorge, Twin Sisters, Deep Gorge and the show-stopping Bungle Bungle domes... here we fly ...
The mystery of the banding of the domes:These distinctive cone-like rock formations with striped orange and grey layers are known as the beehive domes. Formed some 350 million years ago, the sedimentary rock has been weathered and eroded by wind and water into these unmissable dome-shaped towers. The dark horizontal bands are caused by cyanobacteria - a microbial community that has formed on the outer surface of the rock, and the orange bands are caused by the presence of iron and manganese oxides in the sandstone. This protective coating is only a few millimetres thick but helps stabilise the fragile domes and slow down further erosion. Osmand Range 1400 M yrs old - Sandstone & dolomiteBungle Bungle Range 360 M yrs old - Sandstone & conglomerateOrd River Valley 2 M yrs old - Limestone, sandstone & sandstone
Purnululu Conservation Park
Piccaninny Gorge Trek
Characterised by white sand, rounded pebbles, and some rocky sections artfully sculptured by the forces of water, Piccaninny Creek bed is an attraction in its own right. Majestic sandstone domes, orange coloured rock walls and the ever-blue Kimberley sky round off this picture-perfect scenery.
The 'sculptured' creek bed of Picaninny Creek
Leigh carrying supplies for 22 travellers ...
Heading towards Cathedral Gorge
A great place for reflection about life ...
Cathedral Gorge is a world-famous natural arena, equal in size to a cathedral and rivalling the acoustics of an opera house. How I would have loved to hear Renato Dolcini sing here...
Embraced by vertical, deeply undercut rock walls, the massive amphitheatre is humbling in its grandeur.
Bellburn Airstrip
Purnululu from the air with HeliSpirit
A30 Bungle Bungle Domes & Red Rock Gorges Flight over Red Rock Gorge, Piccanniny Gorge, Twin Sisters, Deep Gorge and the show-stopping Bungle Bungle domes... here we fly ...
The mystery of the banding of the domes:
These distinctive cone-like rock formations with striped orange and grey layers are known as the beehive domes. Formed some 350 million years ago, the sedimentary rock has been weathered and eroded by wind and water into these unmissable dome-shaped towers. The dark horizontal bands are caused by cyanobacteria - a microbial community that has formed on the outer surface of the rock, and the orange bands are caused by the presence of iron and manganese oxides in the sandstone. This protective coating is only a few millimetres thick but helps stabilise the fragile domes and slow down further erosion.
Osmand Range 1400 M yrs old - Sandstone & dolomite
Bungle Bungle Range 360 M yrs old - Sandstone & conglomerateOrd River Valley 2 M yrs old - Limestone, sandstone & sandstone
Back at the airstrip
Another sunset over the Bungle Bungle Range
After a-never-to-forget experience, we ended this most memorable day with a glass of bubbles and everlasting memories.
This concludes Part 1 of our Kimberley Trip.