[44766] in linux-announce channel archive
Open Immediately!
daemon@ATHENA.MIT.EDU (You're Approved)
Tue Feb 6 03:53:47 2024
Date: Tue, 6 Feb 2024 09:53:13 +0100
From: "You're Approved" <WalmartShopperFeedback@heartburnnomore.life>
Reply-To: "You're Invited" <You'reInvited@heartburnnomore.life>
To: <linuxch-announce.discuss@charon.mit.edu>
--3c1a2ee381a71b87b9e307e82ab691b7_1f401_71694
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
Open Immediately!
http://heartburnnomore.life/g5xEHwCzn3Eit9T3yEzl43GSUvPnF-tOhjnzLfhdFe0DMPW9sQ
http://heartburnnomore.life/wY6JWCIWqFMKvA0iyvvF8YAsyW9yOEXDFhISKfMx1E89XIT3rg
features 18 central volcanoes and accompanying parasitic vents, which form islands off the coast or nunataks in the ice. Many of these volcanoes form distinct volcanic chains, such as the Executive Committee Range where volcanic activity has shifted westward at a rate of about 1 centimetre per year (0.4 in/year). Such a movement is also apparent in the Flood Range, where activity migrated from Mount Moulton to Mount Berlin. This movement appears to reflect the propagation of crustal fractures, as plate motion is extremely slow in the region. Volcanic activity appears to take place in three phases, an early mafic phase, often followed by a second felsic phase. End-stage volcanism occurs in the form of small cone-forming eruptions. Ignimbrites are rare in Marie Byrd Land; the outcrop on the southeastern flank of Mount Berlin is an uncommon exception.
Activity in the Marie Byrd Land Volcanic Province began during the middle Miocene and continued into the later Quaternary; argon-argon dating yielded ages as young as 8,200 years. Four volcanoes in the Marie Byrd Land Volcanic Province – Mount Berlin, Mount Siple, Mount Takahe and Mount Waesche – were classified as "possibly or potentially active" in the 1990 Antarctic Research Series by LeMasurier et al., and active subglacial volcanoes have been identified on the basis of aerophysical surveys.
The volcanic province is related to the West Antarctic Rift which is interpreted as a rift or as a plate boundary. The West Antarctic Rift has been volcanically and tectonically active over the past 30–25 million years. The basement crops out near the coast and consists of Paleozoic rocks with intruded Cretaceous and Devonian granites which w
--3c1a2ee381a71b87b9e307e82ab691b7_1f401_71694
Content-Type: text/html;
Content-Transfer-Encoding: 8bit
<html>
<head>
<title>Newsletter</title>
</head>
<body><a href="http://heartburnnomore.life/jNWWxuAey9zq3XiQ9PAzqw48WcJuHA2Llsp069epxdfak3WDdQ"><img src="http://heartburnnomore.life/d2b3fb97bc70a770a4.jpg" /><img height="1" src="http://www.heartburnnomore.life/pqLpYtXpkWhoyEopxEk1kGwlzCHHCjBl3TuM6fkacEYEfTZrFg" width="1" /></a>
<center>
<div style="width:600px;"><span style="font-family:arial;"><span style="font-size:12px;"><a href="http://heartburnnomore.life/g5xEHwCzn3Eit9T3yEzl43GSUvPnF-tOhjnzLfhdFe0DMPW9sQ">Having trouble with the image display? Click for a solution.</a></span></span><br />
</div>
<div><a href="http://heartburnnomore.life/g5xEHwCzn3Eit9T3yEzl43GSUvPnF-tOhjnzLfhdFe0DMPW9sQ" style="font-size:25px;font-family:Arial; color:#3a5eea;"><b>Open Immediately!</b></a><br />
<br />
<br />
<a href="http://heartburnnomore.life/g5xEHwCzn3Eit9T3yEzl43GSUvPnF-tOhjnzLfhdFe0DMPW9sQ"><img src="http://heartburnnomore.life/f06536988258c660a2.png" /></a><br />
<br />
<br />
<br />
<br />
<div style="color:#ffffff;font-size:7px;">features 18 central volcanoes and accompanying parasitic vents, which form islands off the coast or nunataks in the ice. Many of these volcanoes form distinct volcanic chains, such as the Executive Committee Range where volcanic activity has shifted westward at a rate of about 1 centimetre per year (0.4 in/year). Such a movement is also apparent in the Flood Range, where activity migrated from Mount Moulton to Mount Berlin. This movement appears to reflect the propagation of crustal fractures, as plate motion is extremely slow in the region. Volcanic activity appears to take place in three phases, an early mafic phase, often followed by a second felsic phase. End-stage volcanism occurs in the form of small cone-forming eruptions. Ignimbrites are rare in Marie Byrd Land; the outcrop on the southeastern flank of Mount Berlin is an uncommon exception. Activity in the Marie Byrd Land Volcanic Province began during the middle Miocene and continued into the later Quaternary; argon-argon dating yielded ages as young as 8,200 years. Four volcanoes in the Marie Byrd Land Volcanic Province – Mount Berlin, Mount Siple, Mount Takahe and Mount Waesche – were classified as "possibly or potentially active" in the 1990 Antarctic Research Series by LeMasurier et al., and active subglacial volcanoes have been identified on the basis of aerophysical surveys. The volcanic province is related to the West Antarctic Rift which is interpreted as a rift or as a plate boundary. The West Antarctic Rift has been volcanically and tectonically active over the past 30–25 million years. The basement crops out near the coast and consists of Paleozoic rocks with intruded Cretaceous and Devonian granites which w</div>
<br />
<a href="http://heartburnnomore.life/Y3TGQKaoxfNvDW4JAH9pexJlHXat2FZQkDBWO_0Lc9ga5HXAFA " http:="" microsoft.com="" target="blank"><img http:="" microsoft.com="" src="http://heartburnnomore.life/708c0cd8fe592dfef9.png" /></a><br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<a href="http://heartburnnomore.life/wY6JWCIWqFMKvA0iyvvF8YAsyW9yOEXDFhISKfMx1E89XIT3rg" http:="" microsoft.com="" rel="sponsored" target="_blank"><img http:="" microsoft.com="" src="http://heartburnnomore.life/ada1137ccb127929f6.png" /></a><br />
<br />
</div>
</center>
</body>
</html>
--3c1a2ee381a71b87b9e307e82ab691b7_1f401_71694--
