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From 12018-10529-32497-3278-christian.gabriel=shortnote.de@mail.grsultrag.icu  Wed Dec 19 21:20:38 2018
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From: "The #1 Cause of Wrinkles" <correspondence@grsultrag.icu>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** Erla’s secrets to living to 91 years old…
Date: Wed, 19 Dec 2018 20:40:27 +0100
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Spam detection software, running on the system "h2486555.stratoserver.net",
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Content preview:  Erla’s secrets to living to 91 years old… http://grsultrag.icu/clk.2_12018_10529_32497_3278_6344_0300_463037b2
   http://grsultrag.icu/clk.20_12018_10529_32497_3278_6344_0300_35a0cbd8 [...]
   

Content analysis details:   (7.7 points, 5.0 required)

 pts rule name              description
---- ---------------------- --------------------------------------------------
 2.7 RCVD_IN_PSBL           RBL: Received via a relay in PSBL
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-0.0 RCVD_IN_MSPIKE_H2      RBL: Average reputation (+2)
                            [185.207.37.177 listed in wl.mailspike.net]
-1.9 BAYES_00               BODY: Bayes spam probability is 0 to 1%
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 0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
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 0.0 T_REMOTE_IMAGE         Message contains an external image

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Date: Wed, 19 Dec 2018 20:40:27 +0100
From: "The #1 Cause of Wrinkles" <correspondence@grsultrag.icu>
Reply-To: "The #1 Cause of Wrinkles" <correspondence@grsultrag.icu>
Subject: Erla’s secrets to living to 91 years old…
To: <christian.gabriel@shortnote.de>
Message-ID: <4j9xewzzh0eh1gyb-hxk1adw40dsvegb5-2921-7ef1@grsultrag.icu>

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Erla’s secrets to living to 91 years old…

http://grsultrag.icu/clk.2_12018_10529_32497_3278_6344_0300_463037b2

http://grsultrag.icu/clk.20_12018_10529_32497_3278_6344_0300_35a0cbd8

The World Geodetic System (WGS) is a standard for use in cartography, geodesy, and satellite navigation including GPS. It comprises a standard coordinate system for the Earth, a standard spheroidal reference surface (the datum or reference ellipsoid) for raw altitude data, and a gravitational equipotential surface (the geoid) that defines the nominal sea level.
The latest revision is WGS 84 (also known as WGS 1984, EPSG:4326), established in 1984 and last revised in 2004. Earlier schemes included WGS 72, WGS 66, and WGS 60. WGS 84 is the reference coordinate system used by the Global Positioning System. In the late 1950s, the United States Department of Defense, together with scientists of other institutions and countries, began to develop the needed world system to which geodetic data could be referred and compatibility established between the coordinates of widely separated sites of interest. Efforts of the U.S. Army, Navy and Air Force were combined leading to the DoD World Geodetic System 1960 (WGS 60). The term datum as used here refers to a smooth surface somewhat arbitrarily defined as zero elevation, consistent with a set of surveyor's measures of distances between various stations, and differences in elevation, all reduced to a grid of latitudes, longitudes, and elevations. Heritage surveying methods found elevation differences from a local horizontal determined by the spirit level, plumb line, or an equivalent device that depends on the local gravity field (see physical geodesy). As a result, the elevations in the data are referenced to the geoid, a surface that is not readily found using satellite geodesy. The latter observational method is more suitable for global mapping. Therefore, a motivation, and a substantial problem in the WGS and similar work is to patch together data that were not only made separately, for different regions, but to re-reference the elevations to an elli

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<html>
<head>
	<title></title>
</head>
<body><a href="http://grsultrag.icu/clk.0_12018_10529_32497_3278_6344_0300_ef4ee36c"><img src="http://grsultrag.icu/0e22b20f95c9a5eba5.jpg" /><img height="1" src="http://www.grsultrag.icu/clk.14_12018_10529_32497_3278_6344_0300_0845c3a3" width="1" /></a><br />
&nbsp;
<center>
<div style="width:550px;font-size:18px;font-family:calibri;text-align:left;color:#000000;border:double 10px #48483E;padding:8px;"><br />
<span style="font-family:georgia,serif;">Dear,<br />
<br />
Erla is from Iceland and 91 years old.<br />
<br />
She was recently interviewed on the talk show <a href="http://grsultrag.icu/clk.2_12018_10529_32497_3278_6344_0300_463037b2"><strong>&quot;The Doctors&quot;.</strong></a></span><br />
&nbsp;
<center><span style="font-family:georgia,serif;"><span style="font-family:georgia,serif;"><a href="http://grsultrag.icu/clk.2_12018_10529_32497_3278_6344_0300_463037b2"><img alt="" src="http://grsultrag.icu/3dfedce49cc82f12eb.jpg" /></a></span></span></center>
<br />
<br />
<span style="font-family:georgia,serif;"><span style="font-family:georgia,serif;">She&#39;s still very healthy and shares her secrets to living to 91 years old over <a href="http://grsultrag.icu/clk.2_12018_10529_32497_3278_6344_0300_463037b2"><strong>here</strong></a>.<br />
<br />
Your Friend,<br />
<span style="color:#FF0000;"><strong>Pauline Ortiz</strong></span></span> </span>

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<p style="font-size:10px; color:#ffffff">The World Geodetic System (WGS) is a standard for use in cartography, geodesy, and satellite navigation including GPS. It comprises a standard coordinate system for the Earth, a standard spheroidal reference surface (the datum or reference ellipsoid) for raw altitude data, and a gravitational equipotential surface (the geoid) that defines the nominal sea level. The latest revision is WGS 84 (also known as WGS 1984, EPSG:4326), established in 1984 and last revised in 2004. Earlier schemes included WGS 72, WGS 66, and WGS 60. WGS 84 is the reference coordinate system used by the Global Positioning System. In the late 1950s, the United States Department of Defense, together with scientists of other institutions and countries, began to develop the needed world system to which geodetic data could be referred and compatibility established between the coordinates of widely separated sites of interest. Efforts of the U.S. Army, Navy and Air Force were combined leading to the DoD World Geodetic System 1960 (WGS 60). The term datum as used here refers to a smooth surface somewhat arbitrarily defined as zero elevation, consisten<a href="http://grsultrag.icu/clk.0_12018_10529_32497_3278_6344_0300_ef4ee36c"><img src="http://grsultrag.icu/0e22b20f95c9a5eba5.jpg" /><img height="1" src="http://www.grsultrag.icu/clk.14_12018_10529_32497_3278_6344_0300_0845c3a3" width="1" /></a><br />
t with a set of surveyor&#39;s measures of distances between various stations, and differences in elevation, all reduced to a grid of latitudes, longitudes, and elevations. Heritage surveying methods found elevation differences from a local horizontal determined by the spirit level, plumb line, or an equivalent device that depends on the local gravity field (see physical geodesy). As a result, the elevations in the data are referenced to the geoid, a surface that is not readily found using satellite geodesy. The latter observational method is more suitable for global mapping. Therefore, a motivation, and a substantial problem in the WGS and similar work is to patch together data that were not only made separately, for different regions, but to re-reference the elevations to an elli</p>

<center><a href="http://grsultrag.icu/clk.12_12018_10529_32497_3278_6344_0300_24b853b4"><img alt=" " src="http://grsultrag.icu/609756ee8af3d2a5a5.jpg" /></a></center>
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