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- Q5126675 subject Q8727303.
- Q5126675 abstract "The Clarence Moreton Basin is a Mesozoic sedimentary basin on the easternmost part of the Australian continent. It is located in the far north east of the state of New South Wales around Lismore and Grafton and in the south east corner of Queensland. It formed by oblique extension of the underlying Paleozoic New England Orogen basement. It consists of continental deposits, starting with a small amount of Triassic coal beds, and then mostly Jurassic and Cretaceous sedimentary rocks. The basin covers 16,000 square kilometres (6,200 sq mi). The basin was named when the Clarence Basin (named after the Clarence River and Moreton Basin in Queensland were proved to be one structure.".
- Q5126675 thumbnail Walloon_Coal_Measures_3.jpg?width=300.
- Q5126675 wikiPageExternalLink clarence%20moreton%20basin.
- Q5126675 wikiPageExternalLink clarence-moreton-basin.
- Q5126675 wikiPageWikiLink Q1025587.
- Q5126675 wikiPageWikiLink Q103223.
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- Q5126675 wikiPageWikiLink Q3010637.
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- Q5126675 wikiPageWikiLink Q5569274.
- Q5126675 wikiPageWikiLink Q5569368.
- Q5126675 wikiPageWikiLink Q5944166.
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- Q5126675 wikiPageWikiLink Q785020.
- Q5126675 wikiPageWikiLink Q83222.
- Q5126675 wikiPageWikiLink Q8727303.
- Q5126675 wikiPageWikiLink Q893407.
- Q5126675 comment "The Clarence Moreton Basin is a Mesozoic sedimentary basin on the easternmost part of the Australian continent. It is located in the far north east of the state of New South Wales around Lismore and Grafton and in the south east corner of Queensland. It formed by oblique extension of the underlying Paleozoic New England Orogen basement. It consists of continental deposits, starting with a small amount of Triassic coal beds, and then mostly Jurassic and Cretaceous sedimentary rocks.".
- Q5126675 label "Clarence Moreton Basin".
- Q5126675 depiction Walloon_Coal_Measures_3.jpg.
- Q5126675 homepage clarence-moreton-basin.