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Top MD: If You're Constipated Fiber Can Be Deadly
daemon@ATHENA.MIT.EDU (John)
Mon Dec 15 04:55:51 2025
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Date: Mon, 15 Dec 2025 10:35:22 +0100
From: "John" <Reynaldo@lottwochamp.click>
Reply-To: "John" <Alan@lottwochamp.click>
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Top MD: If You're Constipated Fiber Can Be Deadly
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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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Hi,<br />
<br />
If you've been using fiber to relieve constipation, I've got scary news from America's top gut specialist...<br />
<br />
<b>Fiber is likely making things MUCH WORSE.</b><br />
<br />
Taking fiber when constipated is like adding more cars to a traffic jam.<br />
<br />
<i>It grinds poop to a halt and backs up your entire digestive system causing smelly gas, embarrassing bloating, burps, bad breath, acid reflux…</i><br />
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And the accumulation of 10 to 15 pounds of dry hardened feces in your colon.<br />
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Once this happens, it can be impossible to get poop moving again.<br />
<br />
Connecticut MD, Dr. Joe Feuerstein, spent 10 years looking for a solution and discovered this…<br />
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Tracey C. from Frazeysburg, OH said: "I got a full release the same day I used this. Now I’m going number two like clockwork and I feel so much lighter, energized and comfortable all day!"<br />
<br />
John<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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