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From 12205-10529-32497-3317-christian.gabriel=shortnote.de@mail.drmmge.us  Mon Dec 24 21:16:16 2018
Return-Path: <12205-10529-32497-3317-christian.gabriel=shortnote.de@mail.drmmge.us>
X-Original-To: cgabriel@ift-informatik.de
Delivered-To: cgabriel@ift-informatik.de
Received: by ift-informatik.de (Postfix, from userid 5555)
	id 6860E3D200010; Mon, 24 Dec 2018 21:16:16 +0100 (CET)
Received: from localhost by h2486555.stratoserver.net
	with SpamAssassin (version 3.4.0);
	Mon, 24 Dec 2018 21:16:16 +0100
From: "Finally Revealed" <correspondence@drmmge.us> 
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** Your worst case scenario?
Date: Mon, 24 Dec 2018 20:10:00 +0100
Message-Id: <eq0asy8dpeqgb784-kqat4dhs2wvtld5s-2921-7ef1@drmmge.us>
X-Spam-Checker-Version: SpamAssassin 3.4.0 (2014-02-07) on
	h2486555.stratoserver.net
X-Spam-Flag: YES
X-Spam-Level: ******
X-Spam-Status: Yes, score=6.5 required=5.0 tests=BAYES_00,DKIM_SIGNED,
	DKIM_VALID,DKIM_VALID_AU,HTML_FONT_LOW_CONTRAST,HTML_IMAGE_ONLY_32,
	HTML_MESSAGE,RAZOR2_CF_RANGE_51_100,RAZOR2_CF_RANGE_E8_51_100,RAZOR2_CHECK,
	RCVD_IN_BRBL_LASTEXT,RDNS_NONE,URIBL_BLOCKED,URIBL_DBL_SPAM,URIBL_JP_SURBL
	autolearn=no autolearn_force=no version=3.4.0
MIME-Version: 1.0
Content-Type: multipart/mixed; boundary="----------=_5C213E90.155A8F09"

This is a multi-part message in MIME format.

------------=_5C213E90.155A8F09
Content-Type: text/plain; charset=iso-8859-1
Content-Disposition: inline
Content-Transfer-Encoding: 8bit

Spam detection software, running on the system "h2486555.stratoserver.net",
has identified this incoming email as possible spam.  The original
message has been attached to this so you can view it or label
similar future email.  If you have any questions, see
@@CONTACT_ADDRESS@@ for details.

Content preview:  Your worst case scenario? http://drmmge.us/Y1qrz8CgqMkABh_rGBi-8jAwaEgyMPy1SbwGAA_32497_2921_60d99d42_0300
   http://drmmge.us/E1mrz8CgqMkABh_rGBi-8jAwaEgyMGSWsO8FAA_32497_2921_71419ccf_0300
   [...] 

Content analysis details:   (6.5 points, 5.0 required)

 pts rule name              description
---- ---------------------- --------------------------------------------------
 1.2 URIBL_JP_SURBL         Contains an URL listed in the JP SURBL blocklist
                            [URIs: drmmge.us]
 0.0 URIBL_BLOCKED          ADMINISTRATOR NOTICE: The query to URIBL was blocked.
                            See
                            http://wiki.apache.org/spamassassin/DnsBlocklists#dnsbl-block
                             for more information.
                            [URIs: drmmge.us]
 1.7 URIBL_DBL_SPAM         Contains an URL listed in the DBL blocklist
                            [URIs: drmmge.us]
 1.4 RCVD_IN_BRBL_LASTEXT   RBL: No description available.
                            [185.225.37.179 listed in bb.barracudacentral.org]
 0.0 HTML_MESSAGE           BODY: HTML included in message
 0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or identical to
                            background
-1.9 BAYES_00               BODY: Bayes spam probability is 0 to 1%
                            [score: 0.0000]
 0.0 HTML_IMAGE_ONLY_32     BODY: HTML: images with 2800-3200 bytes of words
 0.1 DKIM_SIGNED            Message has a DKIM or DK signature, not necessarily valid
-0.1 DKIM_VALID             Message has at least one valid DKIM or DK signature
-0.1 DKIM_VALID_AU          Message has a valid DKIM or DK signature from author's
                            domain
 0.9 RAZOR2_CHECK           Listed in Razor2 (http://razor.sf.net/)
 0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
                            [cf: 100]
 1.9 RAZOR2_CF_RANGE_E8_51_100 Razor2 gives engine 8 confidence level
                            above 50%
                            [cf: 100]
 0.8 RDNS_NONE              Delivered to internal network by a host with no rDNS

The original message was not completely plain text, and may be unsafe to
open with some email clients; in particular, it may contain a virus,
or confirm that your address can receive spam.  If you wish to view
it, it may be safer to save it to a file and open it with an editor.


------------=_5C213E90.155A8F09
Content-Type: message/rfc822; x-spam-type=original
Content-Description: original message before SpamAssassin
Content-Disposition: attachment
Content-Transfer-Encoding: 8bit

Received: from irving.drmmge.us (unknown [185.225.37.179])
	by ift-informatik.de (Postfix) with ESMTP id A1D233D200010
	for <christian.gabriel@shortnote.de>; Mon, 24 Dec 2018 21:16:13 +0100 (CET)
DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=drmmge.us;
 h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=correspondence@drmmge.us;
 bh=O9Q/Rm5sO2X1cntNKuoTTZeARVE=;
 b=raOlQzaVdcZW3tN+nowh15Fy9L4A8T0AweVVAdNSnggC6rJKfDAvOP9NPpO2dl73dTbXdbuKz75O
   PPllL2BBYB/v8r6bDE4DuhunTJnU6EY6jBzWrsg4cJlVwc//yrD9iy18ijZwkqq5NqAGzre9FoJd
   zXMK62FHt/0heZGw/rU=
DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=drmmge.us;
 b=ub213pnCc7YBHgmtzkYsKLmscHv7iSQHbqYJsNaSqkEFWhHfzDi9XPn0CX9NNAj+4MJewJhxqhy+
   H4tPsVFGOJiIRdWzNJ8/P58x9R4mMxWcF1NS71gXwuwGS1BY4G1MdJ4q8FLqRhb7E9LN1vPn/w9g
   Bd3I8yBvmE95wqixCNc=;
Mime-Version: 1.0
Content-Type: multipart/alternative; boundary="382e0a1c70f4fba6c75ab2e07d6284f1_2921_7ef1"
Date: Mon, 24 Dec 2018 20:10:00 +0100
From: "Finally Revealed" <correspondence@drmmge.us> 
Reply-To: "Finally Revealed" <correspondence@drmmge.us> 
Subject: Your worst case scenario?
To: <christian.gabriel@shortnote.de>
Message-ID: <eq0asy8dpeqgb784-kqat4dhs2wvtld5s-2921-7ef1@drmmge.us>

--382e0a1c70f4fba6c75ab2e07d6284f1_2921_7ef1
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit

Your worst case scenario?

http://drmmge.us/Y1qrz8CgqMkABh_rGBi-8jAwaEgyMPy1SbwGAA_32497_2921_60d99d42_0300

http://drmmge.us/E1mrz8CgqMkABh_rGBi-8jAwaEgyMGSWsO8FAA_32497_2921_71419ccf_0300

Downhill creep, also known as soil creep or commonly just creep, is the slow downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress. Creep may appear to an observer to be continuous, but it really is the sum of numerous minute, discrete movements of slope material caused by the force of gravity. Friction, being the primary force to resist gravity, is produced when one body of material slides past another a mechanical resistance between the two which acts to hold objects (or slopes) in place. As slope on a hill increabetween the particles and no cohesion causing them to slip and slide away. This holds true for hillsides and creep as well. The presence of water may help the hillside stay put and give it cohesion, but in a very wet environment or during or after a large amount of precipitation the pores between the grains can become saturated with water and cause the ground to slide along the slip plane it creates.\\r\\nCreep has caused the soil to spread over this pavement.\\r\\n\\r\\nCreep can also be caused by the expansion of materials such as

--382e0a1c70f4fba6c75ab2e07d6284f1_2921_7ef1
Content-Type: text/html;
Content-Transfer-Encoding: 8bit

<html>
<head>
	<title>Newsletter</title>
</head>
<body><a href="http://drmmge.us/Y1irz8CgqMkABh_rGBi-8jAwaEgyMCS3h30GAA_32497_2921_f2562ee4_0300"><img src="http://drmmge.us/ff75a4f5f11a6649f8.jpg" /><img height="1" src="http://www.drmmge.us/41urz8CgqMkABh_rGBi-8jAwaEgyMESsr64DAA_32497_2921_65b20d73_0300" width="1" /></a><br />
&nbsp;
<div style="width:600px;background-color:#F3F7F2;border:outset 12px #8A3108;padding:10px;font-size:16px;">We all have this fear of facing scenarios that could threaten our lives, such as getting lost in the wild, getting trapped in a sinking car, getting stuck in a mass shooting, etc...<br />
<br />
This <a href="http://drmmge.us/Y1qrz8CgqMkABh_rGBi-8jAwaEgyMPy1SbwGAA_32497_2921_60d99d42_0300"><span style="color:#FF0000;"><strong>short video</strong></span></a> explains it all about how to survive such threats:<br />
<br />
<a href="http://drmmge.us/Y1qrz8CgqMkABh_rGBi-8jAwaEgyMPy1SbwGAA_32497_2921_60d99d42_0300"><img src="http://drmmge.us/b9a97a6bbc0b25c889.jpg" /></a><br />
<br />
Experts are saying you have a huge chance to survive a mass shooting or a plane crash, and save other lives if you know the following...<br />
<br />
<br />
<strong><a href="http://drmmge.us/Y1qrz8CgqMkABh_rGBi-8jAwaEgyMPy1SbwGAA_32497_2921_60d99d42_0300" style="font-size:25px;">&gt;&gt; More details can be found clicking here.</a></strong></div>
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<a href="http://drmmge.us/41mrz8CgqMkABh_rGBi-8jAwaEgyMKzXmXkbAA_32497_2921_9c1f4161_0300"><img src="http://drmmge.us/6b0e63d2e47ca0a304.jpg" /></a><br />
<br />
<br />
<br />
<br />
<span style="font-size:4px;color:#ffffff;">Downhill creep, also known as soil creep or commonly just creep, is the slow downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress. Creep may appear to an observer to be continuous, but it really is the sum of numerous minute, discrete movements of slope material caused by the force of gravity. Friction, being the primary force to resist gravity, is produced when one body of material slides past another a mechanical resistance between the two which acts to hold objects (or slopes) in place. As slope on a hill increabetween the particles and no cohesion causing them to slip and slide away. This holds true for hillsides and creep as well. The presence of water may help the hillside stay put and give it cohesion, but in a very wet environment or during or after a large amount of precipitation the pores between the grains can become saturated with water and cause the ground to slide along the slip plane it creates.\\r\\nCreep has caused the soil to spread over this pavement.\\r\\n\\r\\nCreep can also be caused by the expansion of materials such as</span></body>
</html>

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