[191889] in SIPB-AFS-requests
I have not had any mosquitoes in my bedroom since I got this.
daemon@ATHENA.MIT.EDU (Revolutionary Product)
Fri Apr 24 07:27:52 2020
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Date: Fri, 24 Apr 2020 07:27:51 -0400
From: "Revolutionary Product" <RevolutionaryProduct@moskidiy.live>
Reply-To: "Kill Insects" <RevolutionaryProduct@moskidiy.live>
Subject: I have not had any mosquitoes in my bedroom since I got this.
To: <sipb-afsreq-mtg@charon.mit.edu>
Message-ID: <ss9ipbxmhyl0yz95-oaervcba5p2fh7hp-27c-15e89@moskidiy.live>
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I have not had any mosquitoes in my bedroom since I got this.
http://moskidiy.live/IFxMJrIDFIew_cwyXI0gza-GDHfuwP4gqdTpluJ73bWaqf4
http://moskidiy.live/GaI61eUJr7ad5AIS9ORIbFJnf4b6oDZpJuYuZ9xApE1_AoI
rock layers above. Much of the lower continental crust is metamorphic, except for recent igneous intrusions. Horizontal tectonic movements such as the collision of continents create orogenic belts, and cause high temperatures, pressures and deformation in the rocks along these belts. If the metamorphosed rocks are later uplifted and exposed by erosion, they may occur in long belts or other large areas at the surface. The process of metamorphism may have destroyed the original features that could have revealed the rock's previous history. Recrystallization of the rock will destroy the textures and fossils present in sedimentary rocks. Metasomatism will change the original composition.
Regional metamorphism tends to make the rock more indurated and at the same time to give it a foliated, shistose or gneissic texture, consisting of a planar arrangement of the minerals, so that platy or prismatic minerals like mica and hornblende have their longest axes arranged parallel to one another. For that reason many of these rocks split readily in one direction along mica-bearing zones (schists). In gneisses, minerals also tend to be segregated into bands; thus there are seams of quartz and of mica in a mica schist, very thin, but consisting essentially of one mineral. Along the mineral layers composed of soft or fissile minerals the rocks will split most readily, and the freshly split specimens will appear to be faced or coated with this mineral; for example, a piece of mica schist looked at facewise might be supposed to consist entirely of shining scales of mica. On the edge of the specimens, however, the white folia of granular quartz will be visible. In gneisses these alternating folia are sometimes thicker and less regular than in schists, but most importantly less micaceous; they may be lenticular, dying out rapidly. Gneisses also, as a rule, contain more feldspar than schists do, and are tougher and less fissile. Contortion or crumbling of the foliation is by no means uncommon; splitting faces are undulose or puckered. Schistosity and gneissic banding (the two main types of foliation) are formed by directed pressure at elevated temperature, and to interstitial movement, or internal flow arranging the mineral particles while they are crystallizing in that directed pressure field.
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<h1><a href="http://moskidiy.live/IFxMJrIDFIew_cwyXI0gza-GDHfuwP4gqdTpluJ73bWaqf4">BREAKING: Amazing Invention For UV Light to Rid Homes of Insects For Good</a></h1>
<a href="http://moskidiy.live/IFxMJrIDFIew_cwyXI0gza-GDHfuwP4gqdTpluJ73bWaqf4"><img src="http://moskidiy.live/c9dcc2630beff09b2c.jpg" /></a>
<p style="font-size:20px;line-height:30px;">There are <b>thousands of different insect</b> repellents on the market, but how many of them actually do what they're supposed to? With recent deadly outbreaks of Malaria, Dengue Fever, and the <b>Zika Germ</b>, millions of people around the world have been scratching their heads trying to find an effective way to deal with the problem.<br />
<br />
While <b>chemical sprays</b> and plug-in repellents might work, they often have a pungent odor, and may even be harmful to your <b>family's health.</b> If a concoction of chemicals can knock out a mosquito problem immediately, what would they be doing to your health as you breathe it in? Surely there must be another way to combat the problem - and we just might have found it.</p>
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<a href="http://moskidiy.live/IFxMJrIDFIew_cwyXI0gza-GDHfuwP4gqdTpluJ73bWaqf4" style="background-color:green;padding:15px;font-size:35px;"><span style="color:#FFFF00;">Check Availability >>></span></a></div>
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<span style="color:#FFFFFF;font-size:10px;">rock layers above. Much of the lower continental crust is metamorphic, except for recent igneous intrusions. Horizontal tectonic movements such as the collision of continents create orogenic belts, and cause high temperatures, pressures and deformation in the rocks along these belts. If the metamorphosed rocks are later uplifted and exposed by erosion, they may occur in long belts or other large areas at the surface. The process of metamorphism may have destroyed the original features that could have revealed the rock's previous history. Recrystallization of the rock will destroy the textures and fossils present in sedimentary rocks. Metasomatism will change the original composition. Regional metamorphism tends to make the rock more indurated and at the same time to give it a foliated, shistose or gneissic texture, consisting of a planar arrangement of the minerals, so that platy or prismatic minerals like mica and hornblende have their longest axes arranged parallel to one another. For that reason many of these rocks split readily in one direction along mica-bearing zones (schists). In gneisses, minerals also tend to be segregated into bands; thus there are seams of quartz and of mica in a mica schist, very thin, but consisting essentially of one mineral. Along the mineral layers composed of soft or fissile minerals the rocks will split most readily, and the freshly split specimens will appear to be faced or coated with this mineral; for example, a piece of mica schist looked at facewise might be supposed to consist entirely of shining scales of mica. On the edge of the specimens, however, the white folia of granular quartz will be visible. In gneisses these alternating folia are sometimes thicker and less regular than in schists, but most importantly less micaceous; they may be lenticular, dying out rapidly. Gneisses also, as a rule, contain more feldspar than schists do, and are tougher and less fissile. Contortion or crumbling of the foliation is by no means uncommon; splitting faces are undulose or puckered. Schistosity and gneissic banding (the two main types of foliation) are formed by directed pressure at elevated temperature, and to interstitial movement, or internal flow arranging the mineral particles while they are crystallizing in that directed pressure field.</span></center>
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