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Westarctica

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-|style="padding:0 0.9em 0 0;" | [[File:Balchen Glacier - Bruce.jpg|300px]]
+|style="padding:0 0.9em 0 0;" | [[File:Inspecting the GPS antenna at Toney Mountain.jpg|300px]]
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-The '''[[Balchen Glacier]]''' is a [[crevasse|crevassed]] [[glacier]] in [[Antarctica]], flowing west to [[Block Bay]] between the [[Phillips Mountains]] and the [[Fosdick Mountains]] in [[Westarctica]]. It was discovered on December 5, 1929, by the Byrd Antarctic Expedition and named by [[Richard E. Byrd]] in honor of Bernt Balchen, chief pilot of the expedition.
+'''[[Toney Mountain]]''' is an elongated [[snow]]-covered shield volcano, 60 km (38 mi) long and rising to 3,595 meters at Richmond Peak, located 56 km (35 mi) southwest of [[Kohler Range]] in [[Westarctica]].
-Lars Vorländer, a German citizen of Westarctica, was granted the [[Peerage of Westarctica|peerage title]] [[Duke of the Balchen Glacier]] by Letters Patent on 23 January 2018. In March of that year, the Duke became a prominent patron of the [[Westarctica Civilian Corps]] with the creation of the Vorländer Scholarship.
+Toney Mountain lies in a tectonically and volcanically active region of [[Antarctica]]. There, a layer of basaltic rocks up to 5 kilometers (3.1 mi) thick underlie a series of felsic volcanic edifices. These basaltic rocks in turn are emplaced above a Paleozoic basement with granite intrusions of Devonian-Cretaceous, which crops out in some mountain ranges. Beneath Toney Mountain, the basaltic floor rises from an elevation of 3 kilometers (1.9 mi) beneath sea level, and the volcano is situated on the floor of a graben. The region is further characterized by a 500 by 1,200 kilometers (310 mi × 750 mi) large dome-like uplift, part of the West Antarctic Rift, and it may reflect the presence of a stationary hotspot.
-<p><small>Photographer: Bruce Luyendyk</small></p>
+<p><small>Photo by: Nicolas Bayou, UNAVCO</small></p>
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