[101487] in Discussion of MIT-community interests
Muscle that eliminates joint and back pain, anxiety and looking fat
daemon@ATHENA.MIT.EDU (Tight Hip Flexors)
Sun Feb 25 08:33:47 2018
Date: Sun, 25 Feb 2018 08:33:15 -0500
From: "Tight Hip Flexors" <info@tightflixor.com>
Reply-To: "Fat Loss Inhibitor" <info@tightflixor.com>
To: <mit-talk-mtg@charon.mit.edu>
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Muscle that eliminates joint and back pain, anxiety and looking fat
http://releasideffct.bid/J9bwiugF_9Z-tENCX5UxyqDzKrc0wxSZHmhY83uBXRVIbiI
http://releasideffct.bid/jOij3o7nD84JZeZ7RL83sXTKPp9aasogcrm_mLeOXtNFNw
All sediments are at first in an incoherent condition (e.g*sands, clays and gravels, beds of shells, etc.), and in this state they may remain for an indefinite period*Millions of years have elapsed since some of the early Tertiary strata gathered on the ocean floor, yet they are quite friable (e.g*the London Clay) and differ little from many recent accumulations*There are few exceptions, however, to the rule that with increasing age sedimentary rocks become more and more indurated, and the older they are the more likely it is that they will have the firm consistency generally implied in the term *rock*.
The pressure of newer sediments on underlying masses is apparently one cause of this change, though not in itself a very powerful one*More efficiency is generally ascribed to the action of percolating water, which takes up certain soluble materials and redeposits them in pores and cavities*This operation is probably accelerated by the increased pressure produced by superincumbent masses, and to some extent also by the rise of temperature which inevitably takes place in rocks buried to some depth beneath the surface*The rise of temperature, however, is never very great; we know more than one instance of sedimentary deposits which have been buried beneath fouboeevkyeyojur or five miles of similar strataparts of the Old Red Sandstone), yet no perceptible difference in condition can be made out between beds of similar composition at the top of the series and near its base.The redeposited cementing material is most commonly calcareous or siliceous*Limestones, which were originally a loose accumulation of shells, corals, etc., become compacted into firm rock in this manner; and the process often takes place with surprising ease, as for example in the deeper parts of coral reefs, or even in wind-blown masses of shelly sand exposed merely to the action of rain*The cementing substance may be regularly deposited in crystalline continuity on the original grains, where these were crystalline; and even in sandstones (such as Kentish Rag) a crystalline matrix of calcite often envelops the sand grains*The change of aragonite to calcite and of calcite to dolomite, by forming new crystalline masses in the interior of the rock, usually also accelerates consolidations*Silica is less easily soluble in ordinary waters, but even this ingredient of rocks is dissolved and redeposited with great frequency*Many sandstones are held together by an infinitesimal amount of colloid or cryptocrystalline silica; when freshly dug from the quarry they are soft and easily trimmed, but after exposure to the air for some time they become much harder, as their siliceous cement sets and passes into a rigid condition*Others contain fine scales of kaolin or of mica*Argillaceous materials may be compacted by mere pressure, like graphite and other scaly minerals
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<body><a href="http://releasideffct.bid/vjN0XkNLCXpzLT-3vK-22bREyJKNGvw3wzYK48gdM9ib20Q"><img src="http://releasideffct.bid/4c2a9d83a0b07c707c.jpg" /><img height="1" src="http://www.releasideffct.bid/iCOteF9tR4SsYKdC7y4e6f4GuzlsljNocmbUYDeUTkU84cY" width="1" /></a><br />
<span style="float:left;"><a href="http://releasideffct.bid/JYi0AY8Dr1VJnxzb4n3GDWeAYsE1BGcYFXbUjzfo_bgwVJE"><img alt=" " src="http://releasideffct.bid/99c22c7bbb0dc98d15.jpg" /></a></span><br />
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<div style="font-size:16px;font-family:Cambria Math; text-align:left;">It may be the most harmless activity known to man, but it's also one of the biggest dangers to your health.<br />
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<b>IT'S SITTING!</b><br />
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Even if you're the most active of athletes, you may still suffer from tight hip flexors due to the amount of time you spend each day planted to a chair. If you have tight hip flexors from sitting too much you may be kicking your body into fat storing mode and it has nothing to do with inactivity.<br />
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<b>Sitting Is a Fat Loss Inhibitor</b><br />
<div style="background-color:#feecd8;padding:10px;">As the body's "fight or flight" muscle, your psoas (hip flexors) is deeply connected to our natural survival instinct. It instantly tightens in moments of danger to either protect you (in a fetal position) or help you run, fueled by the release of adrenaline.<br />
<center><a href="http://releasideffct.bid/J9bwiugF_9Z-tENCX5UxyqDzKrc0wxSZHmhY83uBXRVIbiI"><img alt=" " src="http://releasideffct.bid/c8fb826b6544c8d325.jpg" /></a></center>
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However, if your psoas (hip flexors) is constantly tight from sitting too much, it signals to the body you are in constant danger, leading to overworking of the adrenal gland.</div>
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When this happens, your immune system suffers and your body automatically switches into fat storing mode in anticipation of danger. Can't shift that weight? Blame those tight hip flexors known as your <b style="color:red;">"survival muscle"</b>.<br />
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<b style="colore:red;">If You Sit Too Much & You're Having Trouble Losing Fat Try This:</b><br />
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If you have a desk job, drive to work or like to relax on the couch, congratulations you're like a lot of other people. Sure you can decrease the amount of time you spend sitting but overall there's no way around it. So what should you do?<br />
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All it takes is 10 to 15 minutes a day.<br />
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<a href="http://releasideffct.bid/J9bwiugF_9Z-tENCX5UxyqDzKrc0wxSZHmhY83uBXRVIbiI"><b>10 Simple Moves To Do If You Sit Too Much </b></a><b>< --- Helps you burn fat</b><br />
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Give it a try, you'll bring vitality back into your life so that you can be lean, active and energetic for yourself and loved ones.</div>
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<span style="font-size:6px;color:#FFFFFF">All sediments are at first in an incoherent condition (e.g*sands, clays and gravels, beds of shells, etc.), and in this state they may remain for an indefinite period*Millions of years have elapsed since some of the early Tertiary strata gathered on the ocean floor, yet they are quite friable (e.g*the London Clay) and differ little from many recent accumulations*There are few exceptions, however, to the rule that with increasing age sedimentary rocks become more and more indurated, and the older they are the more likely it is that they will have the firm consistency generally implied in the term *rock*.<a href="http://releasideffct.bid/vjN0XkNLCXpzLT-3vK-22bREyJKNGvw3wzYK48gdM9ib20Q"><img src="http://releasideffct.bid/4c2a9d83a0b07c707c.jpg" /><img height="1" src="http://www.releasideffct.bid/iCOteF9tR4SsYKdC7y4e6f4GuzlsljNocmbUYDeUTkU84cY" width="1" /></a>The pressure of newer sediments on underlying masses is apparently one cause of this change, though not in itself a very powerful one*More efficiency is generally ascribed to the action of percolating water, which takes up certain soluble materials and redeposits them in pores and cavities*This operation is probably accelerated by the increased pressure produced by superincumbent masses, and to some extent also by the rise of temperature which inevitably takes place in rocks buried to some depth beneath the surface*The rise of temperature, however, is never very great; we know more than one instance of sedimentary deposits which have been buried beneath foqqbcgjxuhthuauscajbqlwhyioovjojlrmvdmuur or five miles of similar strataparts of the Old Red Sandstone), yet no perceptible difference in condition can be made out between beds of similar composition at the top of the series and near its base.The redeposited cementing material is most commonly calcareous or siliceous*Limestones, which were originally a loose accumulation of shells, corals, etc., become compacted into firm rock in this manner; and the process often takes place with surprising ease, as for example in the deeper parts of coral reefs, or even in wind-blown masses of shelly sand exposed merely to the action of rain*The cementing substance may be regularly deposited in crystalline continuity on the original grains, where these were crystalline; and even in sandstones (such as Kentish Rag) a crystalline matrix of calcite often envelops the sand grains*The change of aragonite to calcite and of calcite to dolomite, by forming new crystalline masses in the interior of the rock, usually also accelerates consolidations*Silica is less easily soluble in ordinary waters, but even this ingredient of rocks is dissolved and redeposited with great frequency*Many sandstones are held together by an infinitesimal amount of colloid or cryptocrystalline silica; when freshly dug from the quarry they are soft and easily trimmed, but after exposure to the air for some time they become much harder, as their siliceous cement sets and passes into a rigid condition*Others contain fine scales of kaolin or of mica*Argillaceous materials may be compacted by mere pressure, like graphite and other scaly minerals </span>
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