From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #16695 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Tuesday, September 16 2025 Volume 14 : Number 16695 Today's Subjects: ----------------- This Gets You High Energy All Day Long! ["Cellular Rejuvenation" Subject: This Gets You High Energy All Day Long! This Gets You High Energy All Day Long! http://sharpknife.click/hOJ9xcZUWdSjsbNvTj-cgYUfpgr6rIrDXz_H5nk4eWwcMIq7eQ http://sharpknife.click/cec_N0lNT9_E1CUSaf9DVxtUumITIUC2FrTHU3GzAMx6GWQRHA nown to harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all of Earth's water is contained in its global ocean, covering 70.8% of Earth's crust. The remaining 29.2% of Earth's crust is land, most of which is located in the form of continental landmasses within Earth's land hemisphere. Most of Earth's land is at least somewhat humid and covered by vegetation, while large ice sheets at Earth's polar deserts retain more water than Earth's groundwater, lakes, rivers, and atmospheric water combined. Earth's crust consists of slowly moving tectonic plates, which interact to produce mountain ranges, volcanoes, and earthquakes. Earth has a liquid outer core that generates a magnetosphere capable of deflecting most of the destructive solar winds and cosmic radiation. Earth has a dynamic atmosphere, which sustains Earth's surface conditions and protects it from most meteoroids and UV-light at entry. It has a composition of primarily nitrogen and oxygen. Water vapor is widely present in the atmosphere, forming clouds that cover most of the planet. The water vapor acts as a greenhouse gas and, together with other greenhouse gases in the atmosphere, particularly carbon dioxide (CO2), creates the conditions for both liquid surface water and water vapor to persist via the capturing of energy from the Sun's light. This process maintains the current average surface temperature of 14.76 B0C (58.57 B0F), at which water is liquid under normal atmospheric pressure. Differences in the amount of captured energy between geographic regions (as with the equato ------------------------------ Date: Tue, 16 Sep 2025 15:07:22 +0200 From: "Never forget anything" Subject: Harvard: This common household toxin triggers memory loss Harvard: This common household toxin triggers memory loss http://brightcraft.za.com/FAh-DorAsExS52TZcIxibqYcevEe--Pe_Sdjz1hRDFnPqsFz http://brightcraft.za.com/buj-Ov2KrxZsdHXmKOzl527h0gKK1v5M4kImf8a-C6kxSEJmoA ools in a magma chamber within the crust below the stratovolcano. The processes that trigger the final eruption remain a question for further research. Possible mechanisms include: Magma differentiation, in which the lightest, most silica-rich magma and volatiles such as water, halogens, and sulfur dioxide accumulate in the uppermost part of the magma chamber. This can dramatically increase pressures. Fractional crystallization of the magma. When anhydrous minerals such as feldspar crystallize out of the magma, this concentrates volatiles in the remaining liquid, which can lead to a second boiling that causes a gas phase (carbon dioxide or water) to separate from the liquid magma and raise magma chamber pressures. Injection of fresh magma into the magma chamber, which mixes and heats the cooler magma already present. This could force volatiles out of solution and lower the density of the cooler magma, both of which increase pressure. There is considerable evidence for magma mixing just before many eruptions, including magnesium-rich olivine crystals in freshly erupted silicic lava that show no reaction rim. This is possible only if the lava erupted immediately after mixing since olivine rapidly reacts with silicic magma to form a rim of pyroxene. Progressive melting of the surrounding country rock. These internal triggers may be modified by external triggers such as sector collapse, earthquakes, or interactions with groundwater. Some of these triggers operate only under limited conditions. For example, sector collapse (where part of the flank of a volcano collapses in a massive landslide) can only trigger the eruption of a very shallow magma chamber. Magma differentiation and thermal expansion also are ineffective as triggers for eruptio ------------------------------ End of alt.music.moxy-fruvous digest V14 #16695 ***********************************************