[47429] in linux-announce channel archive
This Bread Is Breaking Weight Loss Myths
daemon@ATHENA.MIT.EDU (Tibetan Wellness)
Tue Jan 14 06:08:24 2025
Date: Tue, 14 Jan 2025 12:07:52 +0100
From: "Tibetan Wellness" <HealthBreakthroughs@fastleanpros.click>
Reply-To: "Tibetan Wellness" <Bread&Health@fastleanpros.click>
To: <linuxch-announce.discuss@charon.mit.edu>
--aedcdac98f1172ec9f7e68f0dd7bb5d8_2c3b5_13ed1
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
This Bread Is Breaking Weight Loss Myths
Losing weight with bread?
Yes, it is possible but only with this Tibetan bread.
Scientist after scientist has tried to figure out how people who eat this special bread manage to lose weight 11 times faster than keto.
http://fastleanpros.click/fLK4H_EXrDXy-qzhPDOqUCcTykLNvEdT4sOZhih5xs6LTCuwLg
More than 11,500 people have already tried the 5-second Tibetan bread ritual and swear this is the most efficient way to lose stubborn fat.
Discover how easy it is to prepare this Tibetan bread using 2 ingredients found in any kitchen.
Tibetan Bread
http://fastleanpros.click/fLK4H_EXrDXy-qzhPDOqUCcTykLNvEdT4sOZhih5xs6LTCuwLg
ns more than 7 million years. It has taken place during five cycles of magmatic activity, each producing less volcanic material than the previous one. Volcanism during these cycles has created several types of volcanoes, including cinder cones, stratovolcanoes, subglacial volcanoes, shield volcanoes and lava domes. The roughly 1,000-square-kilometre (400-square-mile) volcanic plateau forming the base of the MEVC originated from the successive eruptions of highly mobile lava flows. Volcanic rocks such as basalt, trachybasalt, benmoreite, tristanite, mugearite, trachyte and rhyolite were deposited by multiple eruptions of the MEVC; the latter six rock types are products of varying degrees of magmatic differentiation in underground magma reservoirs. At least 10 distinct flows of obsidian were produced by volcanism of the MEVC, some of which were exploited by indigenous peoples in prehistoric times to make tools and weaponry. Renewed effusive volcanism could block local streams with lava flows whereas renewed explosive volcanism could disrupt air traffic with volcanic ash across parts of northwestern Canada.
The first magmatic cycle took place between 7.5 and 6 million years ago and is represented by the Raspberry, Little Iskut and Armadillo geological formations, each of which is the product of a different eruptive period. Three distinct periods of eruptive activity also characterized the second magmatic cycle between 6 and 1 million years ago; they are represented by the Nido, Spectrum and Pyramid geological formations. The third magmatic cycle about 1 million years ago is represented by the Ice Peak, Pillow Ridge and Edziza geological formations, each of which is also the product of a distinct eruptive period. Three distinct periods of eruptive activity also characterized the fourth magmatic cycle between 0.8 and 0.2 million years ago which are represented by the Arctic Lake, Klastline and Kakiddi geological formations. The fifth magmatic cycle began at least 20,000 years ago and may be ongoing; the single distinct eruptive period of this magmatic cycle is represen
http://fastleanpros.click/by8pwXKXY-jmYAoz6DuyVuEuXUlvMoNYQfcCq-qFoFUP1UAc4w
--aedcdac98f1172ec9f7e68f0dd7bb5d8_2c3b5_13ed1
Content-Type: text/html;
Content-Transfer-Encoding: 8bit
<html>
<head>
<title>Newsletter</title>
</head>
<body><!-- Random comment to confuse filters --><a href="http://fastleanpros.click/WJogWytzTd9gXxOIe1v4FSeQeIgRcwMIMZF-HP40plGbdL1eHQ"><img alt="bot" src="http://fastleanpros.click/faf042216a68203fdc.jpg" /><img alt="bot1" src="http://www.fastleanpros.click/V-YWtc0eXwGXiDQXK4ELD48bz8DjAXEKhEZAdvKmn1_EJvB9Cw" /></a>
<div style="font-family:Arial;font-size:18px;width:550px;padding:10px;">Losing weight with bread?<br />
<br />
Yes, it is possible but only with this Tibetan bread.<br />
<br />
Scientist after scientist has tried to figure out how people who eat this special bread manage to lose weight 11 times faster than keto.<br />
<br />
More than 11,500 people have already tried the 5-second Tibetan bread ritual and swear this is the most efficient way to lose stubborn fat.<br />
<br />
<a href="http://fastleanpros.click/fLK4H_EXrDXy-qzhPDOqUCcTykLNvEdT4sOZhih5xs6LTCuwLg" target="_blank">Discover how easy it is to prepare this Tibetan bread using 2 ingredients found in any kitchen.</a><br />
<br />
<a href="http://fastleanpros.click/fLK4H_EXrDXy-qzhPDOqUCcTykLNvEdT4sOZhih5xs6LTCuwLg" target="_blank"><img alt="Tibetan Bread" src="http://fastleanpros.click/b6487ce54a2e08daac.jpg" /></a><br />
<br />
<br />
<a href="http://fastleanpros.click/P7whWzsDqdZBWmO54UWvjUZD-WZA-7D_ufar5K01jDQnVD510Q" target="_blank"><img alt="Additional Info" src="http://fastleanpros.click/1965eeb31be874c87f.png" /></a> <!-- Random text injection --> <span style="display:none;">abcd1234XYZ5678</span>
<p hidden=""><span style="display:none;">!</span></p>
<div style="font-size:8px;color:#FFFFFF;">ns more than 7 million years. It has taken place during five cycles of magmatic activity, each producing less volcanic material than the previous one. Volcanism during these cycles has created several types of volcanoes, including cinder cones, stratovolcanoes, subglacial volcanoes, shield volcanoes and lava domes. The roughly 1,000-square-kilometre (400-square-mile) volcanic plateau forming the base of the MEVC originated from the successive eruptions of highly mobile lava flows. Volcanic rocks such as basalt, trachybasalt, benmoreite, tristanite, mugearite, trachyte and rhyolite were deposited by multiple eruptions of the MEVC; the latter six rock types are products of varying degrees of magmatic differentiation in underground magma reservoirs. At least 10 distinct flows of obsidian were produced by volcanism of the MEVC, some of which were exploited by indigenous peoples in prehistoric times to make tools and weaponry. Renewed effusive volcanism could block local streams with lava flows whereas renewed explosive volcanism could disrupt air traffic with volcanic ash across parts of northwestern Canada. The first magmatic cycle took place between 7.5 and 6 million years ago and is represented by the Raspberry, Little Iskut and Armadillo geological formations, each of which is the product of a different eruptive period. Three distinct periods of eruptive activity also characterized the second magmatic cycle between 6 and 1 million years ago; they are represented by the Nido, Spectrum and Pyramid geological formations. The third magmatic cycle about 1 million years ago is represented by the Ice Peak, Pillow Ridge and Edziza geological formations, each of which is also the product of a distinct eruptive period. Three distinct periods of eruptive activity also characterized the fourth magmatic cycle between 0.8 and 0.2 million years ago which are represented by the Arctic Lake, Klastline and Kakiddi geological formations. The fifth magmatic cycle began at least 20,000 years ago and may be ongoing; the single distinct eruptive period of this magmatic cycle is represen</div>
<br />
<br />
<!-- More obfuscation --> <a href="http://fastleanpros.click/by8pwXKXY-jmYAoz6DuyVuEuXUlvMoNYQfcCq-qFoFUP1UAc4w" target="_blank"><img alt="Unsubscribe" src="http://fastleanpros.click/34b95807ad75ed6f33.png" /></a><br />
</div>
</body>
</html>
--aedcdac98f1172ec9f7e68f0dd7bb5d8_2c3b5_13ed1--
