Brown Bluff

Volcano located in Antarctica


title: "Brown Bluff" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["tuyas-of-antarctica", "volcanoes-of-graham-land", "landforms-of-trinity-peninsula", "important-bird-areas-of-antarctica", "seabird-colonies", "pleistocene-volcanoes", "penguin-colonies"] description: "Volcano located in Antarctica" topic_path: "general/tuyas-of-antarctica" source: "https://en.wikipedia.org/wiki/Brown_Bluff" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Volcano located in Antarctica ::

::data[format=table title="Infobox mountain"]

FieldValue
nameBrown Bluff
photoBrown Bluff.JPG
photo_captionBrown Bluff as seen from Antarctic Sound
elevation_m745
elevation_ref
listingList of subglacial volcanoes
List of volcanoes in Antarctica
locationTabarin Peninsula, Antarctica
mapAntarctica
labelBrown Bluff
label_positionright
coordinates
coordinates_ref
typeTuya
volcanic_fieldJames Ross Island Volcanic Group
last_eruptionPleistocene
::

| name = Brown Bluff | photo = Brown Bluff.JPG | photo_caption = Brown Bluff as seen from Antarctic Sound | elevation_m = 745 | elevation_ref = | prominence_m = | prominence_ref = | range = | listing = List of subglacial volcanoes List of volcanoes in Antarctica | location = Tabarin Peninsula, Antarctica | map = Antarctica | map_caption = | map_size = | label = Brown Bluff | label_position = right | coordinates = | coordinates_ref = | type = Tuya | volcanic_field= James Ross Island Volcanic Group | age = | last_eruption = Pleistocene | first_ascent = | easiest_route =

Brown Bluff is a basalt tuya on the Tabarin Peninsula of northern Antarctica. It formed in the last 1 million years as a result of subglacial eruptions within an englacial lake. The volcano's original diameter is thought to have been about 12 - and was probably formed by a single vent. Brown Bluff is divided into four stages: pillow volcano, tuff cone, slope failure, and hyaloclastite delta; and into five structural units.

The volcano gets its name from its steep slopes and brown-to-black hyaloclastite. It was applied by the Falkland Islands Dependencies Survey following their survey in 1946.

Environment

Topography

Brown Bluff has a 1.5 km cobble and ash beach rising increasingly steeply towards towering red-brown tuff cliffs embedded with bombs and tephra. The cliffs are heavily eroded, resulting in loose scree and rock falls on higher slopes, and large, wind-eroded boulders on the beach. Permanent ice and tidewater glaciers surround the site to the north and south, occasionally filling the beach with brash ice.

Flora and fauna

Lichens in the genera Xanthoria and Caloplaca have been recorded on exposed boulders from the shoreline to an elevation of 185 m. Mosses occur at higher elevations near glacial drainage.

The site has been identified as an Important Bird Area (IBA) by BirdLife International because it supports a breeding colony of about 20,000 pairs of Adélie penguins, as well as about 550 pairs of gentoo penguins. Other birds nesting there include cape petrels, Wilson's storm petrels and kelp gulls. Weddell seals regularly haul out, and leopard seals often hunt offshore.

Geology

Brown Bluff is a 1/2 mi cliff of volcanic rocks consisting of a tuya or moberg, which is a volcano erupted under an icecap. The base layer is breccia formed by violent phreatic eruptions under the lake formed in the ice cap by the magmatic heat. The middle yellow layers are palagonite weathering of steeply dipping ash layers. The top caprock is composed of black layers are basalt flows that erupted after the meltwater lake drained away, resulting in subaerial lava flows.

References

References

  1. {{usgs-gazetteer
  2. (2013). "Encyclopedia of Quaternary Science". [[Elsevier]].
  3. Skilling, I. P.. (1994). "Evolution of an englacial volcano: Brown Bluff, Antarctica". Bulletin of Volcanology.
  4. (2012). "Brown Bluff". BirdLife International.
  5. Joseph Holliday, Earth Science Department, El Camino College

::callout[type=info title="Wikipedia Source"] This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page. ::

tuyas-of-antarcticavolcanoes-of-graham-landlandforms-of-trinity-peninsulaimportant-bird-areas-of-antarcticaseabird-coloniespleistocene-volcanoespenguin-colonies