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From: "Belly Revolution" <Contact@trimmeriuhrjk.bid>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** Doctors Shocked by Results on Veterans Day....
Date: Mon, 18 Jun 2018 10:31:51 -0400
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Content preview:  Doctors Shocked by Results on Veterans Day.... => http://trimmeriuhrjk.bid/qDAbLM3cpz75YvDYQXv8r9c1cLcdisYyf3eXHEBYBRxy
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Date: Mon, 18 Jun 2018 10:31:51 -0400
From: "Belly Revolution" <Contact@trimmeriuhrjk.bid>
Reply-To: "One trick to lose Fat" <Support@trimmeriuhrjk.bid>
Subject: Doctors Shocked by Results on Veterans Day....
To: <christian.gabriel@shortnote.de>
Message-ID: <fchbghecd3g1cvn6-ivmq8szhqp0q303k-1068@trimmeriuhrjk.bid>

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Doctors Shocked by Results on Veterans Day....

=> http://trimmeriuhrjk.bid/qDAbLM3cpz75YvDYQXv8r9c1cLcdisYyf3eXHEBYBRxy

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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Transitional//EN" "http://www.w3.org/TR/xhtml1/DTD/xhtml1-transitional.dtd">
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<body><a href="http://trimmeriuhrjk.bid/_LLtXwU6gLyZY7ZTCaIK0f10xnAbw9zfGqWvaZE-TSAa"><img border="0" src="http://trimmeriuhrjk.bid/nJ5_yM76VW9beRdCbHQG-0cLImogIrmqtPZCp2avDXaD" /> </a>
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			<p>Dear,</p>

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			<p>Heré it is...</p>

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			<p>Enjoy!</p>

			<p>Regards,<br />
			Paula Andrews</p>

			<hr /></td>
		</tr>
	</tbody>
</table>
<br />
<br />
 
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<table cellpadding="5" cellspacing="0" width="100%">
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			<p align="center" style="text-align:auto;text-align: -webkit-auto;padding-top: inherit;line-height: normal;color: #ffffff;margin-left: inherit;speak-header:once;font-family: Didot,'Didot LT STD','Hoefler Text',Garamond,'Times New Roman',serif;margin-right: none;margin-bottom: 1.4px;padding-top: 1.7px;transition-delay: 0s;margin: default;padding-right: 4.6px;margin-left: 3.9px;cursor: pointer;border-bottom-width:0px;padding-bottom: 4.4px !important;border-left-style:none;padding-left: 3.5px !important;font-size: 10.28px !important;margin-top: 1.5647631px !important;border-bottom-style: none;margin-top: inherit;border-right-style: none;font-style: normal;font-family:inheritmargin-right: 2.9px !important;">Struggles of our Life Islands. The combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a "graticule". The origin/zero point of this system is located in the Gulf of Guinea about 625 km (390 mi) south of Tema, Ghana. Measuring height using datums Main articles: Geodetic datum, Figure of the Earth, and Reference ellipsoid Complexity of the problem To completely specify a location of a topographical feature on, in, or above Earth, one also has to specify the vertical distance from Earth's center or surface. Earth is not a sphere, but an irregular shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0.3% larger than the radius measured through the poles. The shorter axis approximately coincides with the axis of rotation. Though early navigators thought of the sea as a flat surface that could be used as a vertical datum, this is not actually the case. Earth has a series of layers of equal potential energy within its gravitational field. Height is a measurement at right angles to this surface, roughly toward Earth's centre, but local variations make the equipotential layers irregular (though roughly ellipsoidal). The choice of which layer to use for defining height is arbitrary. Common baselines Common height baselines include The surface of the datum ellipsoid, resulting in an ellipsoidal height The mean sea level as described by the gravity geoid, yielding the orthometric height A vertical datum, yielding a dynamic height relative to a known reference height. Along with the latitude {\displaystyle \phi } \phi and longitude {\displaystyle \lambda } \lambda , the height {\displaystyle h} h provides the three-dimensional geodetic coordinates or geographic coordinates for a location. Datums In order to be unambiguous about the direction of "vertical" and the "surface" above which they are measuring, map-makers choose a reference ellipsoid with a given origin and orientation that best fits their need for the area they are mapping. They then choose the most appropriate mapping of the spherical coordinate system onto that ellipsoid, called a terrestrial reference system or geodetic datum. Datums may be global, meaning that they represent the whole earth, or they may be local, meaning that they represent an ellipsoid best-fit to only a portion of the earth. Points on the earth's surface move relative to each other due to continental plate motion, subsidence, and diurnal movement caused by the moon and the tides. This daily movement can be as much as a metre. Continental movement can be up to 10 cm a year, or 10 m in a century. A weather system high-pressure area can cause a sinking of 5 mm. Scandinavia is rising by 1 cm a year as a result of the melting of the ice sheets of the last ice age, but neighbouring Scotland is rising by only 0.2 cm. These changes are insignificant if a local datum is used, but are statistically significant if a global datum is used. Examples of global datums include World Geodetic System (WGS 84), the default datum used for the Global Positioning System,[n 4] and the International Terrestrial Reference Frame (ITRF), used for estimating continental drift and crustal deformation. The distance to Earth's centre can be used both for very deep positions and for positions in space. Local datums chosen by a national cartographical organisation include the North American Datum, the European ED50, and the British OSGB36. Given a location, the datum provides the latitude {\displaystyle \phi } \phi and longitude {\displaystyle \lambda } \lambda . In the United Kingdom there are three common latitude, longitude, and height systems in use. WGS 84 differs at Greenwich from the one used on published maps OSGB36 by approximately 112m. The military system ED50, used by NATO, differs from about 120m to 180m. The latitude and longitude on a map made against a local datum may not be the same as one obtained from a GPS receiver. Coordinates from the mapping system can sometimes be roughly changed into another datum using a simple translation. For example, to convert from ETRF89 (GPS) to the Irish Grid add 49 metres to the east, and subtract 23.4 metres from the north. More generally one datum is changed into any other datum using a process called Helmert transformations. This involves converting the spherical coordinates into Cartesian coordinates and applying a seven parameter transformation (translation, three-dimensional rotation), and converting back. In popular GIS software, data projected in latitude/longitude is often represented as a 'Geographic Coordinate System'. For example, data in latitude/longitude if the datum is the North American Datum of 1983 is denoted by 'GCS North American 1983'. Further information: Geographic coordinate conversion Map projection Main article: Map projection</p>
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