[44969] in linux-announce channel archive
Leaching Vinegar: Pain Relief Secret
daemon@ATHENA.MIT.EDU (Leaching Vinegar)
Wed Feb 28 04:13:59 2024
Date: Wed, 28 Feb 2024 10:08:03 +0100
From: "Leaching Vinegar" <LeachingVinegar@pelvicfloorstrong.za.com>
Reply-To: "Vinegar Secret" <VinegarSecret@pelvicfloorstrong.za.com>
To: <linuxch-announce.discuss@charon.mit.edu>
--958ebbcfaaabcb2ef1e167fb6dc8c5e0_2260a_c97ba
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
Leaching Vinegar: Pain Relief Secret
http://pelvicfloorstrong.za.com/Ly7o00DGy0XLXZDmvWU6ktwdBOB8ioBhuCF_YzHuDHodE1MdQQ
http://pelvicfloorstrong.za.com/tw7QadmwvN2M8LXkMyhhhIuWYpjrVO0UPxZuK3j9tKbCwCX5GA
astern flank of the cone is collapsed. The occurrence of eroded scoria cones and lava domes has been reported. The lava flows reach thicknesses of 2–6 metres (6 ft 7 in – 19 ft 8 in) and lengths of 8 kilometres (5.0 mi), and consist of mafic andesite that defines a calc-alkaline suite. Phenocrysts are mostly amphibole, clinopyroxene and olivine. Rock samples from the volcano have been analyzed.
The volcano erupted 750,000 years ago and is part of the fourth volcanic stage in the region. There are a number of mafic volcanic centres in the southern Puna, including Antofagasta de la Sierra north of Carachipampa. Cerro Blanco farther southwest produced ignimbrites, which cover the terrain southwest of Carachipampa, and is still active. Seismic tomography has identified a low-speed anomaly underneath Carachipampa, which connects to it and to several neighbouring volcanoes like Galán and Ojos del Salado. The so-called "Cerro Galán Magmatic Body" lies north of Carachipampa; the volcano lies above its margin. There is evidence of neotectonic activity at Carachipampa.
Surroundings
The cone lies at the centre, and the lowest point, of a 149 by 64 kilometres (93 mi × 40 mi) wide deserted, vegetation-free plain that is one of the lowest-elevation areas in the Puna. To the west, across a ridge, lies the Incahuasi basin, to the east there is a sharp demarcation with the Campo de Piedra Pomez with numerous yardangs carved into ignimbrites. Permian red beds and Paleogene sediments crop out close to Carachipampa. Other rock formations around the Carachipampa plain range in age from Neoproterozoic over Devonian. The basin is filled with sediments, reaching thicknesses of 700 metres (2,300 ft). The basin is notable for the giant (up to 1.5 metres (4 ft 11 in) high), wind-formed megaripples; they are found southwest of Carachipampa in the valley that runs to Cerro Blanco. Winds have removed fine materials, leaving only granular material on the plain, and eroded sediments from wetlands.
Climate and water
The region has a cold and arid climate, as the A
--958ebbcfaaabcb2ef1e167fb6dc8c5e0_2260a_c97ba
Content-Type: text/html;
Content-Transfer-Encoding: 8bit
<html>
<head>
<title>Newsletter</title>
</head>
<body><a href="http://pelvicfloorstrong.za.com/6_ptFwmQ9WbZvhuS1m-3vqYy-drD8kXlW_79BaYjzYEa4TjGDw"><img src="http://pelvicfloorstrong.za.com/0c6695e3178d899a32.jpg" /><img height="1" src="http://www.pelvicfloorstrong.za.com/wJHDRYLXoOeUp_r0bwbfL1spHZtsQK3pKm7GlPDVfG0DEKxVRQ" width="1" /></a>
<div style="width:550px;font-family:Lucida Fax;font-size:17px;text-align:left;">Hey ,<br />
<br />
You won’t believe how this <a href="http://pelvicfloorstrong.za.com/Ly7o00DGy0XLXZDmvWU6ktwdBOB8ioBhuCF_YzHuDHodE1MdQQ" style="font-weight:bold;">“leaching vinegar” </a>CURES sciatica pain, and aching from arthritis:<br />
<br />
<a href="http://pelvicfloorstrong.za.com/Ly7o00DGy0XLXZDmvWU6ktwdBOB8ioBhuCF_YzHuDHodE1MdQQ" style="font-weight:bold;"><img src="http://pelvicfloorstrong.za.com/93abaa26a47d7c7ce3.png" /></a><br />
<br />
Here’s how it works:<br />
<br />
You pour a small splash of vinegar wherever you hurt…<br />
<br />
<b>Then watch it leach out the toxins that caused your pain in the first place!</b><br />
<br />
There’s no burning, itching, or bad side effects…<br />
<br />
Plus, it takes ONLY a few minutes…<br />
<br />
And it’s probably in your pantry right now!<br />
<br />
<a href="http://pelvicfloorstrong.za.com/Ly7o00DGy0XLXZDmvWU6ktwdBOB8ioBhuCF_YzHuDHodE1MdQQ" style="font-weight:bold;">Click here to see which “leaching vinegar” you need to grab from your pantry</a><br />
<br />
Sincerely,<br />
<br />
<b>Katherine</b></div>
<br />
<br />
<br />
<div style="color:#FFFFFF;font-size:5px;">astern flank of the cone is collapsed. The occurrence of eroded scoria cones and lava domes has been reported. The lava flows reach thicknesses of 2–6 metres (6 ft 7 in – 19 ft 8 in) and lengths of 8 kilometres (5.0 mi), and consist of mafic andesite that defines a calc-alkaline suite. Phenocrysts are mostly amphibole, clinopyroxene and olivine. Rock samples from the volcano have been analyzed. The volcano erupted 750,000 years ago and is part of the fourth volcanic stage in the region. There are a number of mafic volcanic centres in the southern Puna, including Antofagasta de la Sierra north of Carachipampa. Cerro Blanco farther southwest produced ignimbrites, which cover the terrain southwest of Carachipampa, and is still active. Seismic tomography has identified a low-speed anomaly underneath Carachipampa, which connects to it and to several neighbouring volcanoes like Galán and Ojos del Salado. The so-called "Cerro Galán Magmatic Body" lies north of Carachipampa; the volcano lies above its margin. There is evidence of neotectonic activity at Carachipampa. Surroundings The cone lies at the centre, and the lowest point, of a 149 by 64 kilometres (93 mi × 40 mi) wide deserted, vegetation-free plain that is one of the lowest-elevation areas in the Puna. To the west, across a ridge, lies the Incahuasi basin, to the east there is a sharp demarcation with the Campo de Piedra Pomez with numerous yardangs carved into ignimbrites. Permian red beds and Paleogene sediments crop out close to Carachipampa. Other rock formations around the Carachipampa plain range in age from Neoproterozoic over Devonian. The basin is filled with sediments, reaching thicknesses of 700 metres (2,300 ft). The basin is notable for the giant (up to 1.5 metres (4 ft 11 in) high), wind-formed megaripples; they are found southwest of Carachipampa in the valley that runs to Cerro Blanco. Winds have removed fine materials, leaving only granular material on the plain, and eroded sediments from wetlands. Climate and water The region has a cold and arid climate, as the A</div>
<br />
<br />
<br />
<br />
<br />
<a href="http://pelvicfloorstrong.za.com/qQjr731DNNijFoMekgSBwm6SynGnRcX425n3PogyA5Lmb2kxbw"><img http:="" microsoft.com="" src="http://pelvicfloorstrong.za.com/ae4d74e6bc27b1e055.png" /></a><br />
</body>
</html>
--958ebbcfaaabcb2ef1e167fb6dc8c5e0_2260a_c97ba--
