Trinity Inlet
navigation channel in Queensland, Australia

The Trinity Inlet is an oceanic inlet which serves as the port for the city of Cairns, Queensland, Australia. The city centre is on the western bank where the inlet meets the Coral Sea.
Location and features
The Trinity Inlet is located in the original delta of the Mulgrave River, which since the Pleistocene flows to a mouth further south. This is because Volcanic activity which resulted in the rise of Green Hill near the Mulgrave Valley, did not block the river, as sediments from more local streams continued to build up over the volcanic rocks. The Mulgrave River enters the sea at Russell Heads, approximately 30 km south of Trinity Inlet. It is unlikely that a river would shift its course and add a further 30km to its length before entering the sea. This is because the river would then adopt a shallower gradient and lose efficiency in transporting sediment. Rivers in this region do occasionally shift course (such as the Barron River in the 1930s) but this is usually to adopt a shorter course to the sea and gain a steeper gradient otherwise known as a gradient advantage.
Trinity Inlet is lined with mangroves and mudflats. Within the inlet a large mud island has been formed and was given the name Admiralty Island.
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Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Jul 30, 2026. The linked authority identifier is Q7842862. Authority coordinates are -16.920, 145.784. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.
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This entry incorporates text from “Trinity Inlet” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.