We have the skill set to offer a complete package solution, from planning a shoot through to filming, editing and the high-quality digital production of full length documentaries, online video, and TV commercials. Since the onset of covid We also shoot unique art, culture, science and tourism content. Our knowledge about where, when and how to film in Western Australia has been learned over more than two decades. Our clients benefit from our location consulting expertise. Our diverse range of clients includes government agencies, small businesses, big businesses, and everything in between! They all have one thing in common — they want the type of rare and amazing footage that only Riggs Australia can provide. Hover to scroll through logos. We discovered a killer whale hotspot in the Bremer Bay canyon in before founding killer whale expeditions to this amazing and remote location.
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Located 10 minutes north of Augusta, Jewel Cave is the largest show cave in Western Australia and also the most recently developed. It is named after the Jewel Casket, a small chamber in the lower sections of the cave. The cave was opened to the public on the 26th December Cliff was lowered into the cave during January Descending 12 metres through a solution pipe into a large chamber he reached a soil cone another 8 metres below the ceiling.
The cave has a depth of 42 metres, with the floor being approximately 24 metres above sea level. Jewel Cave is located in a limestone area approximately 90 kilometres long and 3 kilometres wide known as the Leeuwin-Naturaliste Ridge. The limestone Aeolian calcarenite , which forms the Leeuwin- Naturaliste Ridge was formed from coastal sand dunes when westerly winds along our coastline blew beach sand, sea-shells and corals into huge sand dunes during the last million years.
The sand has been cemented together to form limestone by the action of rainwater. A speleothem, or cave decoration, from Jewel Cave was dated at , years old. The uranium-thorium dating establishes a minimum age for speleothem development within the cave — hence the deposition of the limestone must predate this, presumably by a considerable amount. However a sample of limestone was taken from the basal marine unit in Jewel Cave and yielded an age of , years through thermo-luminescence dating.
This data suggests that the limestone may be older than Middle Pleistocene approximately 1 million years ago. A huge chamber is encountered as you enter the cave and several tree roots can be seen spiraling down from the roof as you reach the top platform.
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vegetation along the coast (associated with the Leeuwin Naturaliste National Park) and in the east Figure IW pH scale and the acidity of common solutions Historic heritage places date from the time of European settlement in WA.
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Jorgensen, Diane Clare Quaternary stratigraphy, palaeowinds and palaeoenvironments of carbonate aeolianite on the Garden Island Ridge and in the Naturaliste-Leeuwin region, southwest Western Australia. PhD thesis, James Cook University. Deposition of carbonate aeolianite has long been constrained by research models based on the isolated carbonate platforms of Bermuda and the Bahamas; however, models for Quaternary carbonate aeolianites differ depending on the interplay of several key factors that reflect location-specific circumstances.
Consequently, real steps forward in carbonate aeolianite research require that the depositional system profile e. Accordingly, these parameters are targeted in this research of carbonate aeolianite in the distally steepened ramp-like setting of Western Australia. The research conducted here is focussed on the Tamala Limestone of Western Australia, which is known for the thickest intervals of Pleistocene carbonate aeolianite in Australia and the most extensive aeolianite deposit of this age in the world Ward, ; Brooke, Quaternary deposits in Western Australia form a complex depositional system composed of carbonate aeolianite, protosols, palaeosols, calcretes and marine deposits formed during different glacioeustatic sea levels.
Two regions within the Tamala Limestone are investigated in this research, the Garden Island Ridge within the Perth region and the Naturaliste-Leeuwin region of the Margaret River area. The laterally discontinuous nature of the dune packages and the lack of distinctive marker horizons make unravelling the sedimentary sequence of the aeolian deposits complicated.
To improve understanding of carbonate aeolianite transportation, deposition and preservation and the impact of these processes on the depositional model, the strategy employed here involves interrogation of the dune packages set within a chronostratigraphic framework. The temporal framework for this study is acquired through the application of whole-rock amino acid racemisation AAR dating.
The depositional system profile of the Rottnest Shelf and the AAR dates of aeolian samples indicate that the formation of dunes on the Garden Island Ridge were linked to stands of sea level higher than at least ii the present 40 m isobath.