[226867] in SIPB-AFS-requests
"Ammo shaming" in Walmart (warning for gun owners)
daemon@ATHENA.MIT.EDU (Discreet Carry Gear)
Tue Apr 8 09:53:22 2025
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Date: Tue, 8 Apr 2025 15:53:20 +0200
From: "Discreet Carry Gear" <DiscreetCarryGear@denticore.za.com>
Reply-To: "VNSH Tactical Team" <VNSHMagSolutions@denticore.za.com>
Subject: "Ammo shaming" in Walmart (warning for gun owners)
To: <sipb-afsreq-mtg@charon.mit.edu>
Message-ID: <fqxiyjyfx8hn6yk7-uinqrszpnqerut1z-2c395-5176f@denticore.za.com>
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"Ammo shaming" in Walmart (warning for gun owners)
http://denticore.za.com/WJqwBYkpY32cn3OZh7EuZFz0qOC1p_z7ikW59CQ0R7HHtgAEQg
http://denticore.za.com/mkJgVCCgzzemV-gJVmGewyNZ9DWZDzVXELsOsnD_pHLTE9PvWw
e sheets grounded below sea level inherently become less stable as they melt due to Archimedes' principle. Effectively, these marine ice sheets must have enough mass to exceed the mass of the seawater displaced by the ice, which requires excess thickness. As the ice sheet melts and becomes thinner, the weight of the overlying ice decreases. At a certain point, sea water could force itself into the gaps which form at the base of the ice sheet, and marine ice sheet instability (MISI) would occur.
Even if the ice sheet is grounded below the sea level, MISI cannot occur as long as there is a stable ice shelf in front of it. The boundary between the ice sheet and the ice shelf, known as the grounding line, is particularly stable if it is constrained in an embayment. In that case, the ice sheet may not be thinning at all, as the amount of ice flowing over the grounding line would be likely to match the annual accumulation of ice from snow upstream. Otherwise, ocean warming at the base of an ice shelf tends to thin it through basal melting. As the ice shelf becomes thinner, it exerts less of a buttressing effect on the ice sheet, the so-called back stress increases and the grounding line is push
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<p>As much as it may p*ss you off... if you walk into Walmart carrying your gun, plus a spare mag or two...<strong><em>and they aren't really well concealed...</em></strong><br />
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Chances are good that you're gonna get some looks -- maybe even get<strong>"ammo shamed"</strong> by a nosy soccer mom.<br />
<br />
<strong<a href="http://denticore.za.com/WJqwBYkpY32cn3OZh7EuZFz0qOC1p_z7ikW59CQ0R7HHtgAEQg" http:="" microsoft.com="" rel="sponsored" style="text-decoration: underline; color:#098AF5" target="blank">That's why we wanted to show you the VNSH MagMate -- which lets you <u>conceal virtually any mag right in your pocket,</u> without anyone having a clue!<br />
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<div style="color:#FFFFFF;font-size:10px;">e sheets grounded below sea level inherently become less stable as they melt due to Archimedes' principle. Effectively, these marine ice sheets must have enough mass to exceed the mass of the seawater displaced by the ice, which requires excess thickness. As the ice sheet melts and becomes thinner, the weight of the overlying ice decreases. At a certain point, sea water could force itself into the gaps which form at the base of the ice sheet, and marine ice sheet instability (MISI) would occur. Even if the ice sheet is grounded below the sea level, MISI cannot occur as long as there is a stable ice shelf in front of it. The boundary between the ice sheet and the ice shelf, known as the grounding line, is particularly stable if it is constrained in an embayment. In that case, the ice sheet may not be thinning at all, as the amount of ice flowing over the grounding line would be likely to match the annual accumulation of ice from snow upstream. Otherwise, ocean warming at the base of an ice shelf tends to thin it through basal melting. As the ice shelf becomes thinner, it exerts less of a buttressing effect on the ice sheet, the so-called back stress increases and the grounding line is push</div>
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