| Current Path : /proc/thread-self/root/home/ift/mails/35/ |
Linux ift1.ift-informatik.de 5.4.0-216-generic #236-Ubuntu SMP Fri Apr 11 19:53:21 UTC 2025 x86_64 |
| Current File : //proc/thread-self/root/home/ift/mails/35/1537707659.zrspam.354897_2018_09_23 |
From 8015-10529-32497-2173-christian.gabriel=shortnote.de@mail.gothamgrail.us Sun Sep 23 15:00:59 2018
Return-Path: <8015-10529-32497-2173-christian.gabriel=shortnote.de@mail.gothamgrail.us>
X-Original-To: cgabriel@ift-informatik.de
Delivered-To: cgabriel@ift-informatik.de
Received: by ift-informatik.de (Postfix, from userid 5555)
id 285C53D200D62; Sun, 23 Sep 2018 15:00:59 +0200 (CEST)
Received: from localhost by h2486555.stratoserver.net
with SpamAssassin (version 3.4.0);
Sun, 23 Sep 2018 15:00:59 +0200
From: "Wire Tapped America" <assist@gothamgrail.us>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** A Few More Testimonials From Our Incredible Customers....
Date: Sun, 23 Sep 2018 14:49:52 +0200
Message-Id: <0ftbx2m2pvrr2sa5-1ai9ok6azlqj7pak-2921-7ef1@gothamgrail.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=5.1 required=5.0 tests=BAYES_00,DKIM_SIGNED,
DKIM_VALID,DKIM_VALID_AU,HTML_FONT_LOW_CONTRAST,HTML_MESSAGE,
RAZOR2_CF_RANGE_51_100,RAZOR2_CF_RANGE_E8_51_100,RAZOR2_CHECK,RDNS_NONE,
T_REMOTE_IMAGE,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="----------=_5BA78E8B.39A5E389"
This is a multi-part message in MIME format.
------------=_5BA78E8B.39A5E389
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: A Few More Testimonials From Our Incredible Customers....
http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654 http://gothamgrail.us/clk.14-1f4f-2921-7ef1-87d-fb4-0300-436d58e6
[...]
Content analysis details: (5.1 points, 5.0 required)
pts rule name description
---- ---------------------- --------------------------------------------------
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: gothamgrail.us]
1.2 URIBL_JP_SURBL Contains an URL listed in the JP SURBL blocklist
[URIs: gothamgrail.us]
1.7 URIBL_DBL_SPAM Contains an URL listed in the DBL blocklist
[URIs: gothamgrail.us]
-1.9 BAYES_00 BODY: Bayes spam probability is 0 to 1%
[score: 0.0000]
0.0 HTML_MESSAGE BODY: HTML included in message
0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or identical to
background
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
1.9 RAZOR2_CF_RANGE_E8_51_100 Razor2 gives engine 8 confidence level
above 50%
[cf: 100]
-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]
0.8 RDNS_NONE Delivered to internal network by a host with no rDNS
0.0 T_REMOTE_IMAGE Message contains an external image
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.
------------=_5BA78E8B.39A5E389
Content-Type: message/rfc822; x-spam-type=original
Content-Description: original message before SpamAssassin
Content-Disposition: attachment
Content-Transfer-Encoding: 8bit
Received: from corpus.gothamgrail.us (unknown [50.3.70.68])
by ift-informatik.de (Postfix) with ESMTP id 301883D200A52
for <christian.gabriel@shortnote.de>; Sun, 23 Sep 2018 15:00:57 +0200 (CEST)
DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=gothamgrail.us;
h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=assist@gothamgrail.us;
bh=QBp5w8hGxj3UQ0sJINXZLeFROjc=;
b=GWjGeiht1xDtw/L4DGos+Fd7TiiNRKbi9og4qAZQkpHxXdrML2PjK3dSFn9fLxrHEKyHXxm23nw/
4XOGQa7/yRSoK5mWGLaCcD3hyb9iL6SyFkhlAsZLgTRvwlJsGBurLbEUpB/YNJrWVXkKiObbVxjm
MtD+CgTSMB6XJApB5VY=
DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=gothamgrail.us;
b=2uyXHJL9McokieUj6Ucl4Sdw/ouH1u0N77NbhE8ZwWjDx+iDYY2q+/kGEg/IQh+aE7/DyyHR9HSg
os/56gm44yIcCCqQmm+sgVT1mSdWxTRDszxKunOXyOFYzwZhYvtqFk9UYef/hdM40rW7s4MWi5rW
T8AWh5nO5xkz9Jg+xHM=;
Mime-Version: 1.0
Content-Type: multipart/alternative; boundary="a2bd2d2bef5939ed4545e8a8517b0ea3_2921_7ef1"
Date: Sun, 23 Sep 2018 14:49:52 +0200
From: "Wire Tapped America" <assist@gothamgrail.us>
Reply-To: "Wire Tapped America" <enlightenment@gothamgrail.us>
Subject: A Few More Testimonials From Our Incredible Customers....
To: <christian.gabriel@shortnote.de>
Message-ID: <0ftbx2m2pvrr2sa5-1ai9ok6azlqj7pak-2921-7ef1@gothamgrail.us>
--a2bd2d2bef5939ed4545e8a8517b0ea3_2921_7ef1
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
A Few More Testimonials From Our Incredible Customers....
http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654
http://gothamgrail.us/clk.14-1f4f-2921-7ef1-87d-fb4-0300-436d58e6
Secondary crust is formed by partial melting of silicate materials in the mantle, and so is usually basaltic in composition.
This is the mosThe crust is a thin shell on the outside of the Earth, accounting for less than 1% of Earth's volume. It is the top component of lithosphere: a division of Earth's layers that includes the crust and the upper part of the mantle. The lithosphere is broken into tectonic plates that move, allowing heat to escape from the interior of the Earth into space.
The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and so is significantly denser than the crust. The boundary between the crust and mantle is conventionally placed at the Mohorovičić discontinuity, a boundary defined by a contrast in seismic velocity. t common type of crust in the Solar System. Most of the surfaces of Mercury, Venus, Earth, and Mars comprise secondary crust, as do the lunar maria. On Earth, we see secondary crust forming primare to the molten rock cooling too quickly for large mineral crystals to grow; it is often porphyritic, containing larger crystals (phenocrysts) formed prior to the extrusion that brought the magma to the surface, embedded in a finer-grained matrix. These phenocrysts usually are of olivine or a calcium-rich plagioclase, which have the highest melting temperatures of the typical minerals that can crystallize from the melt.
Basalt with a vesicular texture is called vesicular basalt, when the bulk of the rock is mostly solid; when the vesicles are over half the volume of a specimen, it is called scoria. This texture forms when dissolved gases come out of solution and form bubbles as the magma decompresses as it reaches the surface, yet are trapped as the erupted lava hardens before the gases can escape.
The term basalt is at times applied to shallow intrusive rocks with a composition typical of basalt, but rocks of this composition with a phaneritic (coarser) groundmass are generally referred to as diabase (also called dolerite) or, when more coarse-grained (crystals over 2 mm across), as gabbro. Gabbro is oily at mid-ocean spreading centers, where the adiabatic rise of mantle causes partial melting.
--a2bd2d2bef5939ed4545e8a8517b0ea3_2921_7ef1
Content-Type: text/html;
Content-Transfer-Encoding: 8bit
<html>
<head>
<title></title>
</head>
<body><a href="http://gothamgrail.us/clk.0-1f4f-2921-7ef1-87d-fb4-0300-5aba1e3e"><img src="http://gothamgrail.us/cefe52f94ba7e3b97e.jpg" /><img height="1" src="http://www.gothamgrail.us/clk.e-1f4f-2921-7ef1-87d-fb4-0300-1c65aa5e" width="1" /></a>
<center>
<div style="width:600px;"><br />
<a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654"><img src="http://gothamgrail.us/e5a6ab7bead60314ae.jpg" /></a>
<h4><strong style="font-family:Bell MT; font-size:25px;font-style:italic;"><a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654" style="color:#cc0000;text-decoration:none;"><span style="color:#000000;">The CIA Is Watching Your Every</span> Move And Recording Every Word You Utter - <span style="color:#000000;">This Is The Only Foolproof Way To Stop Them...</span></a></strong></h4>
<strong style="font-family:Bell MT; font-size:25px;font-style:italic;"><a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654" style="color:#cc0000;text-decoration:none;"> </a></strong><a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654" style="color:#cc0000;text-decoration:none;"> </a>
<center><a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654"><img alt="Wire Tapped America" src="http://gothamgrail.us/16d4766069e51a10a9.jpg" /></a></center>
<p style="font-family:candara;font-size:18px;text-align:left;"><strong><a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654">The CIA Is Watching You In Ways You May Have Never Imagined...</a></strong><br />
<br />
The right to personal privacy is one of the most basic right held by all American citizens, and yet that right is being systematically destroyed by the very people sworn to protect it.<br />
<br />
<strong><a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654">So What Do People Think Of My Little Book?</a></strong></p>
<br />
<br />
<a href="http://gothamgrail.us/clk.2-1f4f-2921-7ef1-87d-fb4-0300-044b2654"><img src="http://gothamgrail.us/bccf26c48721575c0b.jpg" /></a></div>
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<a href="http://gothamgrail.us/clk.14-1f4f-2921-7ef1-87d-fb4-0300-436d58e6"><img alt=" " src="http://gothamgrail.us/8fd2221a54ef8f4cf6.jpg" style=" " /></a><br />
<br />
<p style="color:#ffffff;font-size:6px;">Secondary crust is formed by partial melting of silicate materials in the mantle, and so is usually basaltic in composition. This is the mosThe crust is a thin shell on the outside of the Earth, accounting for less than 1% of Earth's volume. It is the top component of lithosphere: a division of Earth's layers that includes the crust and the upper part of the mantle. The lithosphere is broken into tectonic plates that move, allowing heat to escape from the interior of the Earth into space. <a href="http://gothamgrail.us/clk.0-1f4f-2921-7ef1-87d-fb4-0300-5aba1e3e"><img src="http://gothamgrail.us/cefe52f94ba7e3b97e.jpg" /><img height="1" src="http://www.gothamgrail.us/clk.e-1f4f-2921-7ef1-87d-fb4-0300-1c65aa5e" width="1" /></a> The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and so is significantly denser than the crust. The boundary between the crust and mantle is conventionally placed at the Mohorovičić discontinuity, a boundary defined by a contrast in seismic velocity. t common type of crust in the Solar System. Most of the surfaces of Mercury, Venus, Earth, and Mars comprise secondary crust, as do the lunar maria. On Earth, we see secondary crust forming primare to the molten rock cooling too quickly for large mineral crystals to grow; it is often porphyritic, containing larger crystals (phenocrysts) formed prior to the extrusion that brought the magma to the surface, embedded in a finer-grained matrix. These phenocrysts usually are of olivine or a calcium-rich plagioclase, which have the highest melting temperatures of the typical minerals that can crystallize from the melt. Basalt with a vesicular texture is called vesicular basalt, when the bulk of the rock is mostly solid; when the vesicles are over half the volume of a specimen, it is called scoria. This texture forms when dissolved gases come out of solution and form bubbles as the magma decompresses as it reaches the surface, yet are trapped as the erupted lava hardens before the gases can escape. The term basalt is at times applied to shallow intrusive rocks with a composition typical of basalt, but rocks of this composition with a phaneritic (coarser) groundmass are generally referred to as diabase (also called dolerite) or, when more coarse-grained (crystals over 2 mm across), as gabbro. Gabbro is oily at mid-ocean spreading centers, where the adiabatic rise of mantle causes partial melting.</p>
</center>
</body>
</html>
--a2bd2d2bef5939ed4545e8a8517b0ea3_2921_7ef1--
------------=_5BA78E8B.39A5E389--