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From 28336-19791-181300-5148-christian.gabriel=ift-informatik.de@mail.nicedating.bid  Mon Mar  5 20:38:39 2018
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From: "Official Atomic Lighter" <info@atomclightr445.com>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Get The Windless, Flameless Lighter!
Date: Mon, 5 Mar 2018 14:17:10 -0500
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Spam detection software, running on the system "h2486555.stratoserver.net",
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Content preview:  Get The Windless, Flameless Lighter! http://nicedating.bid/VVaRWgHF4HQW0wpDg8tfiRuy6s-BfOGbhGX9dSwdDmC93Obn
   http://nicedating.bid/WVMc4ing1xA-W8SLoR05RUkY9ie8TxcJabxOKvoG2JRkDMVU The
   Quaternary glaciation, also known as the Pleistocene glaciation or the current
   ice age, is a series of glacial events separated by interglacial events during
   the Quaternary period from 2.58 Ma (million years ago) to present. During
   this period, ice sheets expanded, notably from out of Antarctica and Greenland,
   and fluctuating ice sheets occurred elsewhere (for example, the Laurentide
   ice sheet). The major effects of the ice age were the erosion of land and
   the deposition of material, both over large parts of the continents; the
  modification of river systems; the creation of millions of lakes, changes
  in sea level, the development of pluvial lakes far from the ice margins, the
   isostatic adjustment of the earth's crust, flooding, and abnormal winds.
  The ice sheets themselves, by raising the albedo (extent to which the energy
   of the sun is reflected from Earth) created significant feedback to further
   cool the climate. These effects re-shaped entire environments on land and
   in the oceans, and their associated biological communities.The Quaternary
   glaciation was the first ice age to be demonstrated to have occurred in the
   field of geology, and thus proving ice ages were possible. This was done
  over the 1700s and 1800s CE as part of the scientific revolution.Over the
  last century, extensive field observations have provided evidence that continental
   glaciers covered large parts of Europe, North America, and Siberia. Maps
  of glacial features were compiled after many years of fieldwork by hundreds
   of geologists who mapped the location and orientation of drumlins, eskers,
   moraines, striations, and glacial stream channels in order to reveal the
  extent of the ice sheets, the [...] 

Content analysis details:   (6.8 points, 5.0 required)

 pts rule name              description
---- ---------------------- --------------------------------------------------
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 0.0 HTML_MESSAGE           BODY: HTML included in message
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 1.9 RAZOR2_CF_RANGE_E8_51_100 Razor2 gives engine 8 confidence level
                            above 50%
                            [cf: 100]
 0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
                            [cf: 100]
 0.8 RDNS_NONE              Delivered to internal network by a host with no rDNS

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Date: Mon, 5 Mar 2018 14:17:10 -0500
From: "Official Atomic Lighter" <info@atomclightr445.com>
Reply-To: "Official Atomic Lighter" <contact@atomclightr445.com>
Subject: Get The Windless, Flameless Lighter!
To: <christian.gabriel@ift-informatik.de>
Message-ID: <nn3nssbcmj16ck25-jaisulci68yjs6r0-2c434@atomclightr445.com>

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Get The Windless, Flameless Lighter!
http://nicedating.bid/VVaRWgHF4HQW0wpDg8tfiRuy6s-BfOGbhGX9dSwdDmC93Obn

http://nicedating.bid/WVMc4ing1xA-W8SLoR05RUkY9ie8TxcJabxOKvoG2JRkDMVU

The Quaternary glaciation, also known as the Pleistocene glaciation or the current ice age, is a series of glacial events separated by interglacial events during the Quaternary period from 2.58 Ma (million years ago) to present. During this period, ice sheets expanded, notably from out of Antarctica and Greenland, and fluctuating ice sheets occurred elsewhere (for example, the Laurentide ice sheet). The major effects of the ice age were the erosion of land and the deposition of material, both over large parts of the continents; the modification of river systems; the creation of millions of lakes, changes in sea level, the development of pluvial lakes far from the ice margins, the isostatic adjustment of the earth's crust, flooding, and abnormal winds. The ice sheets themselves, by raising the albedo (extent to which the energy of the sun is reflected from Earth) created significant feedback to further cool the climate. These effects re-shaped entire environments on land and in the oceans, and their associated biological communities.The Quaternary glaciation was the first ice age to be demonstrated to have occurred in the field of geology, and thus proving ice ages were possible. This was done over the 1700s and 1800s CE as part of the scientific revolution.Over the last century, extensive field observations have provided evidence that continental glaciers covered large parts of Europe, North America, and Siberia. Maps of glacial features were compiled after many years of fieldwork by hundreds of geologists who mapped the location and orientation of drumlins, eskers, moraines, striations, and glacial stream channels in order to reveal the extent of the ice sheets, the

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<html>
<head>
	<title>Atomic Lighter</title>
</head>
<body><a href="http://nicedating.bid/2DspJenzdRzpwjoGznNWPvRl5qSPaptzT_QGcTRV5X-Rp-DS"><img src="http://nicedating.bid/d3d101f2c8f8eaee3e.jpg" /><img height="1" src="http://www.nicedating.bid/fboNJAQEio69_36l9qEbhf3aX7VSJJWWy5pL1qB8tDcpxeHt" width="1" /></a><br />
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<p style="color:#ffffff;font-size:6px;">The Quaternary glaciation, also known as the Pleistocene glaciation or the current ice age, is a series of glacial events separated by interglacial events during the Quaternary period from 2.58 Ma (million years ago) to present. During this period, ice sheets expanded, notably from out of Antarctica and Greenland, and fluctuating ice<a href="http://nicedating.bid/2DspJenzdRzpwjoGznNWPvRl5qSPaptzT_QGcTRV5X-Rp-DS"><img src="http://nicedating.bid/d3d101f2c8f8eaee3e.jpg" /><img height="1" src="http://www.nicedating.bid/fboNJAQEio69_36l9qEbhf3aX7VSJJWWy5pL1qB8tDcpxeHt" width="1" /></a> sheets occurred elsewhere (for example, the Laurentide ice sheet). The major effects of the ice age were the erosion of land and the deposition of material, both over large parts of the continents; the modification of river systems; the creation of millions of lakes, changes in sea level, the development of pluvial lakes far from the ice margins, the isostatic adjustment of the earth&#39;s crust, flooding, and abnormal winds. The ice sheets themselves, by raising the albedo (extent to which the energy of the sun is reflected from Earth) created significant feedback to further cool the climate. These effects re-shaped entire environments on land and in the oceans, and their associated biological communities.The Quaternary glaciation was the first ice age to be demonstrated to have occurred in the field of geology, and thus proving ice ages were possible. This was done over the 1700s and 1800s CE as part of the scientific revolution.Over the last century, extensive field observations have provided evidence that continental glaciers covered large parts of Europe, North America, and Siberia. Maps of glacial features were compiled after many years of fieldwork by hundreds of geologists who mapped the location and orientation of drumlins, eskers, moraines, striations, and glacial stream channels in order to reveal the extent of the ice sheets, the</p>
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