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Beacon Supergroup information


The Beacon Supergroup and diabase intrusions.
Beacon Supergroup in Taylor Valley. The tan bands are Beacon Sandstone layers and the dark layers are diabase sills, intruded about 180 million years ago.

The Beacon Supergroup is a geological formation exposed in Antarctica and deposited from the Devonian to the Triassic (400 to 250 million years ago). The unit was originally described as either a formation or sandstone, and upgraded to group and supergroup as time passed. It contains a sandy member known as the Beacon Heights Orthoquartzite.[1]

  1. ^ Bradshaw, Margaret A. (August 6, 2013). "The Taylor Group (Beacon Supergroup): the Devonian sediments of Antarctica". Geological Society of London, Special Publications. 81 (1): 67–97. Bibcode:2013GSLSP.381...67B. doi:10.1144/SP381.23. S2CID 128566638. Retrieved December 13, 2013.

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Beacon Supergroup

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basement of granites and gneisses. The sedimentary layers include the Beacon Supergroup sandstones, siltstones, and coal deposited beginning in the Silurian...

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Geology of Antarctica

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Formation, the Crashsite Quartzite, and the Taylor Group within the Beacon Supergroup.: 32–33, 44–47  During the Late Paleozoic icehouse, Antarctica was...

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Ross Sea

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metamorphosed and deformed in the Cretaceous. The Ross Supergroup system and Beacon Supergroup – Ross System rocks exposed in Victoria Land and in the...

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McMurdo Dry Valleys

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the Ross orogeny. The basement complex is overlain by the Jurassic Beacon Supergroup, which is itself intruded by Ferrar Dolerite sheets and sills. The...

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Taylor Valley

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aerial photo at right, the tan bands are sandstone layers from the Beacon Supergroup, a series of sedimentary rock layers formed at the bottom of a shallow...

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Maya Mountain

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the Beacon Supergroup. The Weller Coal Measures form its summit. It is underlain by the Metschel Tillite and the Aztec Siltstone with the Beacon Heights...

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Ross Embayment

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(1981). "History of the Ross Sea region during the deposition of the Beacon Supergroup 400-180 million years ago". Journal of the Royal Society of New Zealand...

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Gangamopteris

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Gangamopteris dominates some coal deposits, such as those of the Beacon Supergroup. In Paleorrota geopark in Rio Grande do Sul, Brazil, were found Gangamopteris...

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Beaconites

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Beaconites is an ichnogenus known from the Beacon Supergroup, Antarctica, comprising a large, segmented burrow, bearing superficial resemblance to the...

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Pensacola Mountains

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succession, and is overlain disconformably by the Dover Sandstone of the Beacon Supergroup. Within the Neptune Group is the Brown Ridge Conglomerate, Elliott...

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Late Paleozoic icehouse

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Land, Antarctica, the Metschel Tillite, made up of reworked Devonian Beacon Supergroup sedimentary strata along with Cambrian and Ordovician granitoids and...

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Cruziana

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arthropods. Cruziana appears in non-marine formations such as the Beacon Supergroup that would have been unsuitable environments for trilobites, and in...

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Cape Fold Belt

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age, which affected the sequence of sedimentary rock layers of the Cape Supergroup in the southwestern corner of South Africa. It was originally continuous...

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Hanson Formation

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(also called Beacon Supergroup) from the Central Transantarctic Mountains was defined by Ferrar in 1907, when he described the "Beacon Sandstone" of...

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Shackleton Range

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sandstones and conglomerates, and is unconformably overlain by the Beacon Supergroup. The range comprises three separate terranes with very different histories...

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The New York Rock and Soul Revue was a musical project supergroup that evolved out of a series of concerts produced and promoted by singer-songwriter Libby...

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Turbidite Hill

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turbidites, which were reportedly found in sedimentary rocks of the Beacon Supergroup which forms the summit of this hill. The exposed bulk of Turbidite...

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Lashly Mountains

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The Lashly Formation is the youngest in the Victoria Group of the Beacon Supergroup. It is a sandstone and siltstone sequence containing plant remains...

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Aztec Mountain

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2.1, approximately 85-metre (279 ft) of sedimentary strata of the Beacon Supergroup are exposed on the eastern flank of Aztec Mountain. Its summit consists...

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Royal Society Range

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Devonian- to Triassic-age sandstones, siltstones and conglomerates of the Beacon Supergroup which dip shallowly westward away from the Ross Sea coast. The entire...

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Mount Joyce

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alternating with rafts of sandstone of the Paleozoic and Mesozoic Beacon Supergroup. The strata dip about 1-2 degrees (at most) to the west. On Mount...

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Tectonic evolution of Patagonia

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passive margin is represented by the Devonian-age lower section of the Beacon Supergroup. Proposed evidence for this connection exists in both the North Patagonian...

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Fremouw Formation

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Stratigraphy and petrology of the mainly fluviatile Permian and Triassic Beacon rocks, Beardmore Glacier area, Antarctica. Ohio State University Institute...

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Lidgettoniopsis Gen. et sp. nov Valid Ryberg, Taylor & Taylor Late Permian Beacon Supergroup (upper Buckley Formation)  Antarctica A seed fern belonging to the...

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List of fossiliferous stratigraphic units in Antarctica

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Hanson Formation Hettangian-Pliensbachian Lashly Formation Carnian Beacon Supergroup Fremouw Formation Early-Late Triassic Buckley Formation Capitanian...

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Geology of the Ellsworth Mountains

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found under the subhorizontal Devonian to Triassic deposits of the Beacon Supergroup, which were produced by Kukri erosional surface near the Transantarctic...

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