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Slash Your Medical Bills Naturally
daemon@ATHENA.MIT.EDU (Plant Power)
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Date: Sat, 7 Jun 2025 18:45:59 +0200
From: "Plant Power" <GreenRemedy@nicoyapuretea.click>
Reply-To: "Green Remedy" <GreenRemedy@nicoyapuretea.click>
Subject: Slash Your Medical Bills Naturally
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Slash Your Medical Bills Naturally
http://nicoyapuretea.click/Yie5Wsxa9oSDfj3cR9XhCtwdOY7hxTk96U7inEBNiWQYtmTLIw
http://nicoyapuretea.click/4QrTv-0NEHB9TFNoFVSpNI9g31a0c7ADpTAwDrQOC9lblyFqxA
aracterized by its nearly ideal 1:1 stoichiometric ratio of magnesium to calcium. It is distinct from high-magnesium limestone in that the magnesium and calcium form ordered layers within the individual dolomite mineral grains, rather than being arranged at random, as they are in high-magnesium calcite grains. In natural dolomite, magnesium is typically between 44 and 50 percent of total magnesium plus calcium, indicating some substitution of calcium into the magnesium layers. A small amount of ferrous iron typically substitutes for magnesium, particularly in more ancient dolomites. Carbonate rock tends to be either almost all calcite or almost all dolomite, with intermediate compositions being quite uncommon.
Dolomite outcrops are recognized in the field by their softness (mineral dolomite has a Mohs hardness of 4 or less, well below common silicate minerals) and because dolomite bubbles feebly when a drop of dilute hydrochloric acid is dropped on it. This distinguishes dolomite from limestone, which is also soft but reacts vigorously with dilute hydrochloric acid. Dolomite usually weathers to a characteristic dull yellow-brown color due to the presence of ferrous iron. This is released and oxidized as the dolomite weathers. Dolomite is usually granular in appearance, with a texture resembling grains of sugar.
Under the microscope, thin sections of dolomite usually show indiv
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<div class="main" style="max-width: 100%;display: block;text-align: left;font-size: 18;font-family: Helvetica;"><strong>What if you could cut down on medical bills by using nature’s medicine instead of tasteless pharmaceutical drugs?</strong><br />
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<div style="color:#FFFFFF;font-size:8px;">aracterized by its nearly ideal 1:1 stoichiometric ratio of magnesium to calcium. It is distinct from high-magnesium limestone in that the magnesium and calcium form ordered layers within the individual dolomite mineral grains, rather than being arranged at random, as they are in high-magnesium calcite grains. In natural dolomite, magnesium is typically between 44 and 50 percent of total magnesium plus calcium, indicating some substitution of calcium into the magnesium layers. A small amount of ferrous iron typically substitutes for magnesium, particularly in more ancient dolomites. Carbonate rock tends to be either almost all calcite or almost all dolomite, with intermediate compositions being quite uncommon. Dolomite outcrops are recognized in the field by their softness (mineral dolomite has a Mohs hardness of 4 or less, well below common silicate minerals) and because dolomite bubbles feebly when a drop of dilute hydrochloric acid is dropped on it. This distinguishes dolomite from limestone, which is also soft but reacts vigorously with dilute hydrochloric acid. Dolomite usually weathers to a characteristic dull yellow-brown color due to the presence of ferrous iron. This is released and oxidized as the dolomite weathers. Dolomite is usually granular in appearance, with a texture resembling grains of sugar. Under the microscope, thin sections of dolomite usually show indiv</div>
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