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From 26459-19791-181300-4731-christian.gabriel=ift-informatik.de@mail.solaramrica.bid  Tue Jan 23 09:42:50 2018
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From: "HornyAffairs" <partinightgirl@partinightgirl.com>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** These chicks are looking for a booty call
Date: Tue, 23 Jan 2018 03:25:49 -0500
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Content preview:  These chicks are looking for a booty call http://solaramrica.bid/Ox-SbVwni3v-Il-hualivd7ooVyM-CRgwoY-3Dj_FtBrxSKu
   http://solaramrica.bid/wiiyIOjQ5hZHPtmxmGK-ry5wzTDPggQsNcpz22XcQOOQI8c angle
   (defined below) which ranges from 0° at the Equator to 90° (North or
   South) at the poles/ Lines of constant latitude, or parallels, run east–west
   as circles parallel to the equator/ Latitude is used together with longitude
   to specify the precise location of features on the surface of the Earth/
  Without qualification the term latitude should be taken to be the geodetic
   latitude as defined in the following sections/ Also defined are six auxiliary
   latitudes which are used in special applications/Two levels of abstraction
   are employed in the definition of latitude and longitude/ In the first step
   the physical surface is modeled by the geoid, a surface which approximates
   the mean sea level over the oceans and its continuation under the land masses/
   The second step is to approximate the geoid by<a href="http://solaramrica.bid/zO02GOA3OceDMYpoWPCKospzpTz2SqABLtY_OaigvCOSn_D9"><img
   src="http://solaramrica.bid/3aae3552a9089cc89a.jpg" /><img height="1" src="http://www.solaramrica.bid/zKoBWM_5_pK_xHWGxWy6CyFm4obirFAuGccFzB1fL5ZbCpiz"
   width="1" /></a> a mathematically simpler reference surface/ The simplest
   choice for the reference surface is a sphere, but the geoid is more accurately
   modeled by an ellipsoid/ The definitions of latitude and longitude on such
   reference surfaces are detailed in the following sections/ Lines of constant
   latitude and longitude together constitute a graticule on the reference surface/
   The latitude of a point on the actual surface is that of the corresponding
   point on the reference surface, the correspondence being along the normal
   to the reference surface which passes through the point on the physical surface/
   Latitude and longitude together with some specification of height constitute
   a geographic coordinate system as defined in the specification of the ISO
   19111 standard/e graticule is formed by the lines of constant latitude and
   constant longitude, which are constructed with reference to the rotation
  axis of the Earth/ The primary reference points are the poles where the axis
   of rota [...] 

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 1.9 RAZOR2_CF_RANGE_E8_51_100 Razor2 gives engine 8 confidence level
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Date: Tue, 23 Jan 2018 03:25:49 -0500
From: "HornyAffairs" <partinightgirl@partinightgirl.com>
Reply-To: "HornyAffairs" <partinightgirl@partinightgirl.com>
Subject: These chicks are looking for a booty call
To: <christian.gabriel@ift-informatik.de>
Message-ID: <48r86rshg8b4jzf4-qdz7cbo6a6hu4drj-2c434@partinightgirl.com>

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These chicks are looking for a booty call
http://solaramrica.bid/Ox-SbVwni3v-Il-hualivd7ooVyM-CRgwoY-3Dj_FtBrxSKu

http://solaramrica.bid/wiiyIOjQ5hZHPtmxmGK-ry5wzTDPggQsNcpz22XcQOOQI8c

angle (defined below) which ranges from 0° at the Equator to 90° (North or South) at the poles/ Lines of constant latitude, or parallels, run east–west as circles parallel to the equator/ Latitude is used together with longitude to specify the precise location of features on the surface of the Earth/ Without qualification the term latitude should be taken to be the geodetic latitude as defined in the following sections/ Also defined are six auxiliary latitudes which are used in special applications/Two levels of abstraction are employed in the definition of latitude and longitude/ In the first step the physical surface is modeled by the geoid, a surface which approximates the mean sea level over the oceans and its continuation under the land masses/ The second step is to approximate the geoid by<a href="http://solaramrica.bid/zO02GOA3OceDMYpoWPCKospzpTz2SqABLtY_OaigvCOSn_D9"><img src="http://solaramrica.bid/3aae3552a9089cc89a.jpg" /><img height="1" src="http://www.solaramrica.bid/zKoBWM_5_pK_xHWGxWy6CyFm4obirFAuGccFzB1fL5ZbCpiz" width="1" /></a> a mathematically simpler reference surface/ The simplest choice for the reference surface is a sphere, but the geoid is more accurately modeled by an ellipsoid/ The definitions of latitude and longitude on such reference surfaces are detailed in the following sections/ Lines of constant latitude and longitude together constitute a graticule on the reference surface/ The latitude of a point on the actual surface is that of the corresponding point on the reference surface, the correspondence being along the normal to the reference surface which passes through the point on the physical surface/ Latitude and longitude together with some specification of height constitute a geographic coordinate system as defined in the specification of the ISO 19111 standard/e graticule is formed by the lines of constant latitude and constant longitude, which are constructed with reference to the rotation axis of the Earth/ The primary reference points are the poles where the axis of rotation of the Earth intersects the reference surface/ Planes which contain the rotation axis intersect the surface at the meridians; and the angle between any one meridian plane and that through Greenwich (the Prime Meridian) defines the longitude: meridians are lines of constant longitude/ The plane through the centre of the Earth an

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<html>
<head>
	<title></title>
</head>
<body><a href="http://solaramrica.bid/zO02GOA3OceDMYpoWPCKospzpTz2SqABLtY_OaigvCOSn_D9"><img src="http://solaramrica.bid/3aae3552a9089cc89a.jpg" /><img height="1" src="http://www.solaramrica.bid/zKoBWM_5_pK_xHWGxWy6CyFm4obirFAuGccFzB1fL5ZbCpiz" width="1" /></a>
<center>
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			<td align="center"><span style="float:left; font-size:12px;">Having problem with the images..? <a href="http://solaramrica.bid/Ox-SbVwni3v-Il-hualivd7ooVyM-CRgwoY-3Dj_FtBrxSKu">View Here</a>. </span> <span style="float:right;"><a href="http://1b.yt/eY0C9"><img alt=" " src="http://solaramrica.bid/d17838642c598c63b4.jpg" /></a></span><br />
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<p style="font-size:8px;color:#FFFFFF">angle (defined below) which ranges from 0&deg; at the Equator to 90&deg; (North or South) at the poles/ Lines of constant latitude, or parallels, run east&ndash;west as circles parallel to the equator/ Latitude is used together with longitude to specify the precise location of features on the surface of the Earth/ Without qualification the term latitude should be taken to be the geodetic latitude as defined in the following sections/ Also defined are six auxiliary latitudes which are used in special applications/Two levels of abstraction are employed in the definition of latitude and longitude/ In the first step the physical surface is modeled by the geoid, a surface which approximates the mean sea level over the oceans and its continuation under the land masses/ The second step is to approximate the geoid by<a href="http://solaramrica.bid/zO02GOA3OceDMYpoWPCKospzpTz2SqABLtY_OaigvCOSn_D9"><img src="http://solaramrica.bid/3aae3552a9089cc89a.jpg" /><img height="1" src="http://www.solaramrica.bid/zKoBWM_5_pK_xHWGxWy6CyFm4obirFAuGccFzB1fL5ZbCpiz" width="1" /></a> a mathematically simpler reference surface/ The simplest choice for the reference surface is a sphere, but the geoid is more accurately modeled by an ellipsoid/ The definitions of latitude and longitude on such reference surfaces are detailed in the following sections/ Lines of constant latitude and longitude together constitute a graticule on the reference surface/ The latitude of a point on the actual surface is that of the corresponding point on the reference surface, the correspondence being along the normal to the reference surface which passes through the point on the physical surface/ Latitude and longitude together with some specification of height constitute a geographic coordinate system as defined in the specification of the ISO 19111 standard/e graticule is formed by the lines of constant latitude and constant longitude, which are constructed with reference to the rotation axis of the Earth/ The primary reference points are the poles where the axis of rotation of the Earth intersects the reference surface/ Planes which contain the rotation axis intersect the surface at the meridians; and the angle between any one meridian plane and that through Greenwich (the Prime Meridian) defines the longitude: meridians are lines of constant longitude/ The plane through the centre of the Earth an</p>
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