[49494] in linux-announce channel archive
Protect Your Home from Pests Without Chemicals
daemon@ATHENA.MIT.EDU (Pest Free Living)
Thu Jul 24 06:16:45 2025
Date: Thu, 24 Jul 2025 05:16:12 -0500
From: "Pest Free Living" <PestFreeLiving@biowave.sa.com>
Reply-To: "Pest Free Living" <ThePestResisterTeam@biowave.sa.com>
To: <linuxch-announce.discuss@charon.mit.edu>
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Protect Your Home from Pests Without Chemicals
http://biowave.sa.com/KwnOgvEEGegIRSQHUn7HiWIem49BW6BFfMAUv2Fy3r48LgOxrw
http://biowave.sa.com/NxBoFqMdf55deQyE3k72fTXyUL0Gl9LpOVVDqNU2JVM3Ty9wGQ
vey reported anomalously hot brines in the central portion of the Red Sea. Later work in the 1960s confirmed the presence of hot, 60 °C (140 °F), saline brines and associated metalliferous muds. The hot solutions were emanating from an active subseafloor rift. Lake Asal in Djibouti is eligible as an experimental site to study the evolution of the deep hot brines of the Red Sea. By observing the strontium isotope composition of the Red Sea brines, it is possible to deduce how these salt waters found at the bottom of the Red Sea could have evolved in a similar way to Lake Asal, which ideally represents their compositional extreme. The high salinity of the waters was not hospitable to living organisms.
Sometime during the Tertiary, the Bab el Mandeb closed and the Red Sea evaporated to an empty hot dry salt-floored sink. Effects causing this would have been:
A "race" between the Red Sea widening and Perim Island erupting filling the Bab el Mandeb with lava.
The lowering of world sea level during the Ice Ages because of much water being locked up in the ice caps.
Several volcanic islands rise from the center of the sea. Most are dormant. However, in 2007, Jabal al-Tair island in the Bab el Mandeb strait erupted violently. Two new islands were formed in 2011 and 2013 in the Zubair Archipelago, a small chain of islands owned by Yemen. The first island, Sholan Island, emerged in an eruption in December 2011, and the second island, Jadid, emerged in Septe
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<div style="color:#FFFFFF;font-size:8px;">vey reported anomalously hot brines in the central portion of the Red Sea. Later work in the 1960s confirmed the presence of hot, 60 °C (140 °F), saline brines and associated metalliferous muds. The hot solutions were emanating from an active subseafloor rift. Lake Asal in Djibouti is eligible as an experimental site to study the evolution of the deep hot brines of the Red Sea. By observing the strontium isotope composition of the Red Sea brines, it is possible to deduce how these salt waters found at the bottom of the Red Sea could have evolved in a similar way to Lake Asal, which ideally represents their compositional extreme. The high salinity of the waters was not hospitable to living organisms. Sometime during the Tertiary, the Bab el Mandeb closed and the Red Sea evaporated to an empty hot dry salt-floored sink. Effects causing this would have been: A "race" between the Red Sea widening and Perim Island erupting filling the Bab el Mandeb with lava. The lowering of world sea level during the Ice Ages because of much water being locked up in the ice caps. Several volcanic islands rise from the center of the sea. Most are dormant. However, in 2007, Jabal al-Tair island in the Bab el Mandeb strait erupted violently. Two new islands were formed in 2011 and 2013 in the Zubair Archipelago, a small chain of islands owned by Yemen. The first island, Sholan Island, emerged in an eruption in December 2011, and the second island, Jadid, emerged in Septe</div>
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