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From 11814-1343-4039405291-3902-christian.gabriel=shortnote.de@mail.aeropency.us Thu Oct 4 22:03:55 2018
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From: "Magic Wand" <manifestation@aeropency.us>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** Magic "Money Wand" Manifests CASH In 24 Hours!
Date: Thu, 4 Oct 2018 21:35:13 +0200
Message-Id: <twusxbemj1bgsseu-bo40uewbglsbhlhn-f0c46eeb@aeropency.us>
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Spam detection software, running on the system "h2486555.stratoserver.net",
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Content preview: This email must be viewed in HTML mode. Hi, If you're struggling
paycheck to paycheck... or feel trapped under a growing mountain of debt...
[...]
Content analysis details: (11.7 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
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[URIs: aeropency.us]
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[64.42.179.234 listed in bl.mailspike.net]
1.2 URIBL_JP_SURBL Contains an URL listed in the JP SURBL blocklist
[URIs: aeropency.us]
0.8 MPART_ALT_DIFF BODY: HTML and text parts are different
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[score: 0.0000]
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0.5 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50%
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0.8 RDNS_NONE Delivered to internal network by a host with no rDNS
0.3 DIGEST_MULTIPLE Message hits more than one network digest check
0.0 LOTS_OF_MONEY Huge... sums of money
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Date: Thu, 4 Oct 2018 21:35:13 +0200
From: "Magic Wand" <manifestation@aeropency.us>
Reply-To: "Magic Wand" <manifestation@aeropency.us>
Subject: Magic "Money Wand" Manifests CASH In 24 Hours!
To: <christian.gabriel@shortnote.de>
Message-ID: <twusxbemj1bgsseu-bo40uewbglsbhlhn-f0c46eeb@aeropency.us>
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<html>
<head>
<title></title>
<style type="text/css">80% {
-webkit-transform: translateX(0%) skewX(-15deg);
transform: translateX(0%) skewX(-15deg);
opacity: 1;
}
100% {
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<body><a href="http://aeropency.us/Rr7JO5RYNRpCs-Czp-5_wTFE1USEINIaviygxxSEbJYjD-iV"><img border="0" src="http://aeropency.us/y14DvrBOahD65Iy7l0lgXRR46y2W9fMAac_rtUi7agymTQ5Z" /> </a>
<div>
<div style="border: 7px hidden #ffffff; width: 600px; background-color: #ffffff">
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<table style="padding-top: 10px;width:600px; font-size:17px;font-family:Palatino Linotype;">
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<td>Hi,<br />
<br />
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</tr>
<tr>
<td align="left" style="font-size:12px;"><br />
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<br />
<a href="http://aeropency.us/jbJvAxnRCwc5ObXnj7uTenZfxZys4XUVIff3LZ72ha_cTXLj"><img alt="Please UnSub_scribe Here!!" src="http://aeropency.us/4f0ba3396a0059a521.jpg" /></a></td>
</tr>
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<table style="width: 620px; background-color: #FFFFFF; border: 5px solid white;">
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<p style=" padding:0px; padding:0px;color:#ffffff; font-size:11px; line-height:-1px">Dependent on local climate, which is affected by the distance to the sea, the exposition and the latitude (from 23°N to 25°S), the altitude varies from 500 m to 4000 m above sea level. Typically, there is a relatively small band of altitude in which the atmospheric environment is suitable for cloud forest development. This is characterized by persistent fog at the vegetation level, resulting in the reduction of direct sunlight and thus of evapotranspiration. Within cloud forests, much of the moisture available to plants arrives in the form of fog drip, where fog condenses on tree leaves and then drips onto the ground below. Annual rainfall can range from 500 to 10,000 mm/year and mean temperature between 8 and 20 °C.<br />
<br />
While cloud forest today is the most widely used term, in some regions, these ecosystems or special types of cloud forests are called mossy forest, elfin forest, montane thicket, and dwarf cloud forest. In comparison with lower tropical moist forests, cloud forests show a reduced tree stature combined with increased stem density and generally the lower diversity of woody plants. Trees in these regions are generally shorter and more heavily stemmed than in lower-altitude forests in the same regions, often with gnarled trunks and branches, forming dense, compact crowns. Their leaves become smaller, thicker and harder with increasing altitude. The high moisture promotes the development of a high biomass and biodiversity of epiphyte, particularly bryophytes, lichens, ferns (including filmy ferns), bromeliads and orchids. The number of endemic plants can be very high.<br />
<br />
An important feature of cloud forests is the tree crowns can intercept the wind-driven cloud moisture, part of which drips to the ground. This fog drip occurs when water droplets from the fog adhere to the needles or leaves of trees or other objects, coalesce into larger drops and then drop to the ground. It can be an important contribution to the hydrologic cycle. Due to the high water content of the soil, the reduced solar radiation and the low rates of decomposition and mineralization, the soil acidity is very high, with more humus and peat often forming the upper soil layer.<br />
<br />
Stadtmüller (1987) distinguishes two general types of tropical montane cloud forests: The definition of cloud forest can be ambiguous, with many countries not using the term (preferring such terms as Afromontane forest and upper montane rain forest, montane laurel forest, or more localised terms such as the Bolivian yungas, and the laurisilva of the Atlantic Islands), and occasionally subtropical and even temperate forests in which similar meteorological conditions occur are considered to be cloud forests. Only 1% of the global woodland consists of cloud forests. Important areas of cloud forest are in Central and South America, East and Central Africa, Indonesia, Malaysia, the Philippines, Papua-New Guinea, and in the Caribbean</p>
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<a href="http://aeropency.us/GJbLV-NReqcmR1w28iubJzQtKKerRPkK5yhQe40bYotDIF2S"><img src="http://aeropency.us/53cee1620d9db84d80.jpg" /></a></div>
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