Difference between revisions of "Template:POTD protected"

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The '''[[2017 - State visit in Scone|2017 State Visit in Scone]]''' was a diplomatic event that occurred between the sovereign of the [[Kingdom of Scone]] and a delegation from [[Westarctica]] in the Niagara Falls region of upstate New York. It was considered an important event in the [[foreign relations of Westarctica]].
The '''Pine Island Glacier''' is a large ice stream, and the fastest melting [[glacier]] in [[Antarctica]], responsible for about 25% of Antarctica's [[ice]] loss. The glacier ice streams flow west-northwest along the south side of the [[Hudson Mountains]] into [[Pine Island Bay]], [[Amundsen Sea]], [[Westarctica]]. It was named in association with Pine Island Bay.


The Westarctica delegation included Grand Duke Travis, the [[Countess of Benton]], and [[Prince-Consort Dinny]]. They met with [[James, King of the Sconnish|King James]] at Old Fort Niagara in Upstate New York, where the King led the visitors on a personal tour of the old battlements.
The area drained by Pine Island Glacier comprises about 10% of the [[West Antarctic Ice Sheet]]. Satellite measurements have shown that the Pine Island Glacier Basin has a greater net contribution of ice to the sea than any other ice drainage basin in the world and this has increased due to recent acceleration of the ice stream. The ice stream is extremely remote, with the nearest continually occupied research station at Rothera, nearly 1,300 km (810 mi) away.


<p><small>Photographer: Fort Niagara Guard</small></p>
<p><small>Photographer: Polargeo</small></p>
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[[:Category:Images|'''(More Featured Images)''']]
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Revision as of 02:30, 13 August 2018

Pine-Island-Fieldcamp.jpg

The Pine Island Glacier is a large ice stream, and the fastest melting glacier in Antarctica, responsible for about 25% of Antarctica's ice loss. The glacier ice streams flow west-northwest along the south side of the Hudson Mountains into Pine Island Bay, Amundsen Sea, Westarctica. It was named in association with Pine Island Bay.

The area drained by Pine Island Glacier comprises about 10% of the West Antarctic Ice Sheet. Satellite measurements have shown that the Pine Island Glacier Basin has a greater net contribution of ice to the sea than any other ice drainage basin in the world and this has increased due to recent acceleration of the ice stream. The ice stream is extremely remote, with the nearest continually occupied research station at Rothera, nearly 1,300 km (810 mi) away.

Photographer: Polargeo

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