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From: "Ketogenic Diet Food" <ketorecipes@creenimcle.us>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** We're shipping your Keto cookbook today
Date: Tue, 24 Apr 2018 16:00:41 +0200
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Content preview: This email must be viewed in HTML mode. There's only a few
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Date: Tue, 24 Apr 2018 16:00:41 +0200
From: "Ketogenic Diet Food" <ketorecipes@creenimcle.us>
Reply-To: "Ketogenic Diet Food" <ketorecipes@creenimcle.us>
Subject: We're shipping your Keto cookbook today
To: <christian.gabriel@shortnote.de>
Message-ID: <3sfthslli78usdhb-vy8i3b66fyg6chs7-f0c46eeb@creenimcle.us>
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<body><a href="http://creenimcle.us/pVbrBRGAN5o9pJxcBjAu9ZQc8_D_KhBjQIU-oACAPyzui9zd"><img border="0" src="http://creenimcle.us/Ry64letIa8YIJGyQIR1sawGDbM2pVK7X46Mz3tz_HTJ_nPaH" /> </a>
<p style=" font-size: 15px; font-family: arial; "> </p>
<p> </p>
<div style=" font-size: 15px; font-family: arial; ">There's only a few left and I wanted to check and see if you wanted this for free but...<br />
<br />
Want to know the secret to pretty much every diet out there? Here it is...<br />
<br />
Most of the time, your body burns carbs for fuel. Any excess carbs you<br />
don't burn are stored as fat. However...<br />
<br />
By limiting your carb and protein intake, you can actually FORCE your<br />
body into a state of "ketosis." In this state, your body "learns"<br />
how to burn fat for fuel. And...<br />
<br />
Get this...<br />
<br />
Almost every diet out there relies on ketosis for fat loss! So...<br />
<br />
How exactly do you get into ketosis? Simple! All you have to do is eat the<br />
keto recipes in this brand new <a href="http://creenimcle.us/5PKZpJ4uN1v8_DBFySxTrj8E0EjInOaa5JdUO8UatX7X2LHW" style="color:#0000FF;"><b>FREE cookbook called The<br />
Wicked Good Ketogenic Diet Cookbook. </b></a>
<p><a href="http://creenimcle.us/5PKZpJ4uN1v8_DBFySxTrj8E0EjInOaa5JdUO8UatX7X2LHW"><img src="http://creenimcle.us/18e5061989540ce051.jpg" /> </a></p>
<br />
This book is jam-packed with 156 delicious fat-shredding ketogenic recipes<br />
that will help you burn fat like crazy. Even stubborn belly and thigh fat won't<br />
stand a chance because your body will have NO CHOICE but to burn that fat for fuel!<br />
<br />
<b>=><a href="http://creenimcle.us/5PKZpJ4uN1v8_DBFySxTrj8E0EjInOaa5JdUO8UatX7X2LHW" style="color:#0000FF;"> You can get your free Wicked Good Keto cookbook right here (just pay s&h)</a></b><br />
<br />
But please hurry since there were only 300 copies printed when they first started<br />
(this print run) they'll likely be gone. Once those books have been claimed,<br />
it could take weeks to get more in stock.<br />
<br />
-Elvira Horton<br />
</div>
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<td colspan="2" style="background-color:#ffffff"><span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:12px">In most earthquakes, the epicenter is the point where the greatest damage takes place, but the length of the subsurface fault rupture may indeed be a long one, and damage can be spread on the surface across the entire rupture zone </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:12px">As an example, in the magnitude 7.9 2002 Denali earthquake in Alaska, the epicenter was at the western end of the rupture, but the greatest damage was about 330 km away at the eastern end </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:12px">During an earthquake, seismic waves propagate in all directions from the hypocenter. Seismic shadowing occurs on the opposite side of the Earth from the earthquake epicenter because the planet's liquid outer core refracts the longitudinal or compressional (P-waves) </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:12px">the transverse or shear waves (S-waves). Outside the seismic shadow zone, both types of wave can be detected but, because of their different velocities and paths through the Earth, they arrive at different times. By measuring the time difference on any seismograph and the distance on a travel-time graph on which the P-wave and S-wave have the same separation, geologists can calculate the distance to the quake's epicenter </span><br />
<br />
<span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif; font-size:12px">his distance is called the epicentral distance, commonly measured in ° (degrees) and denoted as Δ (delta) in seismology. Once distances from the epicenter have been calculated from at least three seismographic measuring stations, the point can be located, using trilateration. </span></td>
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