Welcome To Our Shell

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From 34489-30643-248207-6754-christian.gabriel=ift-informatik.de@mail.marriagirl.bid  Fri Jun 29 11:14:48 2018
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From: "The-Medium-Maria" <contact@marriagirl.bid>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Discover the Key to your Future
Date: Fri, 29 Jun 2018 04:43:33 -0400
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Content preview:  Discover the Key to your Future http://marriagirl.bid/clk.248207-34489-2-30643-6754-13199-4e3c822e-0300
   http://marriagirl.bid/clk.248207-34489-20-30643-6754-13199-a2d91b1f-0300
  [...] 

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---- ---------------------- --------------------------------------------------
 2.7 RCVD_IN_PSBL           RBL: Received via a relay in PSBL
                            [162.244.15.210 listed in psbl.surriel.com]
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Date: Fri, 29 Jun 2018 04:43:33 -0400
From: "The-Medium-Maria" <contact@marriagirl.bid>
Reply-To: "The-Medium-Maria" <info@marriagirl.bid>
Subject: Discover the Key to your Future
To: <christian.gabriel@ift-informatik.de>
Message-ID: <kaj6c3jerkkl3xk2-nbs99g6y0wew2vpq-77b3-3c98f@marriagirl.bid>

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Discover the Key to your Future

http://marriagirl.bid/clk.248207-34489-2-30643-6754-13199-4e3c822e-0300

http://marriagirl.bid/clk.248207-34489-20-30643-6754-13199-a2d91b1f-0300

The first scientific ice drilling expeditions, led by Louis Agassiz from 1840 to 1842, had three goals: to prove that glaciers flowed, to measure the internal temperature of a glacier at different depths, and to measure the thickness of a glacier. Proof of glacier motion was achieved by placed stakes in holes drilled in a glacier and tracking their motion from the surrounding mountain. Drilling through glaciers to determine their thickness, and to test theories of glacier motion and structure, continued to be of interest for some time, but glacier thickness has been measured by seismographic techniques since the 1920s. Although it is no longer necessary to drill through a glacier to determine its thickness, scientists still drill shot holes in ice for these seismic studies. Temperature measurements continue to this day: modelling the behaviour of glaciers requires an understanding of their internal temperature, and in ice sheets, the borehole temperature at different depths can provide information about past climates. Other instruments may be lowered into the borehole, such as piezometers, to measure pressure within the ice, or cameras, to allow a visual review of the stratigraphy. IceCube, a large astrophysical project, required numerous optical sensors to be placed in holes 2.5 km deep, drilled at the South Pole.

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<body><a href="http://marriagirl.bid/clk.248207-34489-0-30643-6754-13199-f428eb6c-0300"><img src="http://marriagirl.bid/1a039b89e83d93bcfc.jpg" /><img height="1" src="http://www.marriagirl.bid/clk.248207-34489-14-30643-6754-13199-7c35dde8-0300" width="1" /></a>&nbsp; &nbsp;
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<div style="width:600px;align:right;"><span style="float:right;font-size:15px;">Images are not showing up correctly.? <a href="http://marriagirl.bid/clk.248207-34489-2-30643-6754-13199-4e3c822e-0300">Click Here.</a> </span><br />
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<span style="color:#FFFFFF;">The first scientific ice drilling expeditions, led by Louis Agassiz from 1840 to 1842, had three goals: to prove that glaciers flowed, to measure the internal temperature of a glacier at different depths, and to measure the thickness of a glacier. Proof of glacier motion was achieved by placed stakes in holes drilled in a glacier and tracking their motion from the surrounding mountain. Drilling through glaciers to determine their thickness, and to test theories of glacier motion and structure, continued to be of interest for some time, but glacier thickness has been measured by<a href="http://marriagirl.bid/clk.248207-34489-0-30643-6754-13199-f428eb6c-0300"><img src="http://marriagirl.bid/1a039b89e83d93bcfc.jpg" /><img height="1" src="http://www.marriagirl.bid/clk.248207-34489-14-30643-6754-13199-7c35dde8-0300" width="1" /></a> seismographic techniques since the 1920s. Although it is no longer necessary to drill through a glacier to determine its thickness, scientists still drill shot holes in ice for these seismic studies. Temperature measurements continue to this day: modelling the behaviour of glaciers requires an understanding of their internal temperature, and in ice sheets, the borehole temperature at different depths can provide information about past climates. Other instruments may be lowered into the borehole, such as piezometers, to measure pressure within the ice, or cameras, to allow a visual review of the stratigraphy. IceCube, a large astrophysical project, required numerous optical sensors to be placed in holes 2.5 km deep, drilled at the South Pole.</span> &nbsp;<br />
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