[50856] in linux-announce channel archive
Why Tea Tree Oil Makes Fungus Impossible To Kill
daemon@ATHENA.MIT.EDU (Health Insider)
Tue Dec 16 11:26:20 2025
Date: Tue, 16 Dec 2025 10:26:15 -0600
From: "Health Insider" <FungusFix@cartsgorilla.ru.com>
Reply-To: "Health Insider" <FungusFix@cartsgorilla.ru.com>
To: <linuxch-announce.discuss@charon.mit.edu>
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Why Tea Tree Oil Makes Fungus Impossible To Kill
http://cartsgorilla.ru.com/7pi8jU8qNC1xdFBqbtLshkkrblHtvsS9B2JMMVAG2NQalHvF
http://cartsgorilla.ru.com/ap7CKhYptulxEdFnZb8AZnh7ayZZfHgNDZBX3GGJHoiSC83j
mally, a temperate glacier is at a melting point throughout the year, from its surface to its base. The ice of a polar glacier is always below the freezing threshold from the surface to its base, although the surface snowpack may experience seasonal melting. A subpolar glacier includes both temperate and polar ice, depending on the depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of a glacier is often described by its basal temperature. A cold-based glacier is below freezing at the ice-ground interface and is thus frozen to the underlying substrate. A warm-based glacier is above or at freezing at the interface and is able to slide at this contact. This contrast is thought to a large extent to govern the ability of a glacier to effectively erode its bed, as sliding ice promotes plucking at rock from the surface below. Glaciers which are partly cold-based and partly warm-based are known as polythermal.
Formation
A glacier cave located on the Perito Moreno Glacier in Argentina
Glaciers form where the accumulation of snow and ice exceeds ablation. A glacier usually originates from a cirque landform (alternatively known as a corrie or as a cwm) - a typically armchair-shaped geological feature (such as a depression between mountains enclosed by arêtes) - which collects and compresses through gravity the snow that falls into it. This snow accumulates and refreezes, turning into névé (granular snow). Further crushing of the individual snowflakes and expelling the air from the snow turns it into firn and eventually "glacial ice". This glacial ice will fill the cirque until it "overflows" through a geological weakness or vacancy from the edge of the cirque called the "lip" or threshold. When the mass of snow and ice reaches sufficient thickness, it begins to move by a com
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<div style="padding:10px;width:602px;font-family:Arial;font-size:18px;text-align:left;"><a href="http://cartsgorilla.ru.com/qR4CZPz1sGqU_ENANzyYju7Xs61S5NglBW2w0BGsokRdL60"><img src="http://cartsgorilla.ru.com/28a1f5f25a966df171.jpg" /><img height="1" src="http://www.cartsgorilla.ru.com/B5zEz-Yku5e_5qXq5L_0u07HZmj33KWZSgmL2RbuNHxFdUw" width="1" /></a><br />
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Scientists at the <b>Infectious Disease Society of America</b> have discovered that tea tree oil can actually worsen foot fungus…<br />
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Making it impossible to kill after you’ve applied the oil on your nails.<br />
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Moreover, it seems that <a href="http://cartsgorilla.ru.com/7pi8jU8qNC1xdFBqbtLshkkrblHtvsS9B2JMMVAG2NQalHvF" http:="" microsoft.com="" rel="sponsored" target="_blank"><b>especially when used like this,</b></a> tea tree oil can destroy your nails in just a couple of hours…<br />
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Click here to find out:<br />
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<a href="http://cartsgorilla.ru.com/7pi8jU8qNC1xdFBqbtLshkkrblHtvsS9B2JMMVAG2NQalHvF" http:="" microsoft.com="" rel="sponsored" target="_blank"><b>Doctors Warn: Tea Tree Oil Actually Makes Fungus Impossible To Kill</b></a><br />
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<span style="color:#FFFFFF; font-size:10px;">mally, a temperate glacier is at a melting point throughout the year, from its surface to its base. The ice of a polar glacier is always below the freezing threshold from the surface to its base, although the surface snowpack may experience seasonal melting. A subpolar glacier includes both temperate and polar ice, depending on the depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of a glacier is often described by its basal temperature. A cold-based glacier is below freezing at the ice-ground interface and is thus frozen to the underlying substrate. A warm-based glacier is above or at freezing at the interface and is able to slide at this contact. This contrast is thought to a large extent to govern the ability of a glacier to effectively erode its bed, as sliding ice promotes plucking at rock from the surface below. Glaciers which are partly cold-based and partly warm-based are known as polythermal.</span> <span style="color:#FFFFFF; font-size:10px;">Formation A glacier cave located on the Perito Moreno Glacier in Argentina Glaciers form where the accumulation of snow and ice exceeds ablation. A glacier usually originates from a cirque landform (alternatively known as a corrie or as a cwm) - a typically armchair-shaped geological feature (such as a depression between mountains enclosed by arêtes) - which collects and compresses through gravity the snow that falls into it. This snow accumulates and refreezes, turning into névé (granular snow). Further crushing of the individual snowflakes and expelling the air from the snow turns it into firn and eventually "glacial ice". This glacial ice will fill the cirque until it "overflows" through a geological weakness or vacancy from the edge of the cirque called the "lip" or threshold. When the mass of snow and ice reaches sufficient thickness, it begins to move by a com</span><br />
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