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From 7771-1348-4018576277-2131-christian.gabriel=shortnote.de@mail.wordweburer.trade Mon Jan 22 15:33:02 2018
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From: "TakeSurveysForCash" <surveys@wordweburer.trade>
To: <christian.gabriel@shortnote.de>
Subject: *****SPAM***** Just got my check for $500.
Date: Mon, 22 Jan 2018 08:31:28 -0600
Message-Id: <wpu2wz0l17geeta8-0xh0xll7b7vf3gho-ef869b95@wordweburer.trade>
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Content preview: This email must be viewed in HTML mode. Secrets To Making
$$$ With Paid Surveys Sometimes people don't believe me when I tell them about
how much you can make taking paid surveys online... [...]
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[162.251.166.66 listed in bb.barracudacentral.org]
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Date: Mon, 22 Jan 2018 08:31:28 -0600
From: "TakeSurveysForCash" <surveys@wordweburer.trade>
Reply-To: "TakeSurveysForCash" <surveys@wordweburer.trade>
Subject: Just got my check for $500.
To: <christian.gabriel@shortnote.de>
Message-ID: <wpu2wz0l17geeta8-0xh0xll7b7vf3gho-ef869b95@wordweburer.trade>
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<body><a href="http://wordweburer.trade/dly9hOAO93angUVCg5ynGiJIzJHsXMfhahUrvI-pIlGUVa1e"><img border="0" src="http://wordweburer.trade/KMXdzKC4KDoIdo5PwMNOaA-Kcrd-tyY6UCo9lGZa08VRNS46" /> </a>
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<p align="center" style="color:#FFF; font-size:30px;font-family: Verdana,Geneva,sans-serif; background-color:#119BE1; padding:5px; border-radius:5px; margin:2px;"><a href="http://wordweburer.trade/-a4CNHQS59gI53ZObkw3Ut4ake73boKxO67lIvkv7ZC8cUQh" style="color:#ffffff;text-decoration:none;"><b>Secrets To Making $$$ With Paid Surveys</b></a></p>
<p><br />
<span style="text-transform: capitalize;">Sometimes people don't believe me when I tell them about how much you can make taking <a href="http://wordweburer.trade/-a4CNHQS59gI53ZObkw3Ut4ake73boKxO67lIvkv7ZC8cUQh">paid surveys online</a>...<br />
<br />
So I took a video of myself actually getting paid $500 for paid surveys to finally set the record straight.</span></p>
<p align="center"><a href="http://wordweburer.trade/-a4CNHQS59gI53ZObkw3Ut4ake73boKxO67lIvkv7ZC8cUQh" style="color:#2879C1;"><img src="http://wordweburer.trade/0c31fe893a71257f5e.jpg" /></a></p>
I'm not going to leave this video up for long, <a href="http://wordweburer.trade/-a4CNHQS59gI53ZObkw3Ut4ake73boKxO67lIvkv7ZC8cUQh">so check it out now</a> before I take it down!<br />
<div align="center" class="submit-wrap" style="text-decoration:none; font-size:60px;"><a href="http://wordweburer.trade/-a4CNHQS59gI53ZObkw3Ut4ake73boKxO67lIvkv7ZC8cUQh"><input type="submit" value="++ Earn #500 for taking a 1 hour paid survey! ++" /></a></div>
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<td align="center" style=" background-color:#119BE1; color:#FFF; border-radius:5px; font-size:20px;"><a href="http://wordweburer.trade/-a4CNHQS59gI53ZObkw3Ut4ake73boKxO67lIvkv7ZC8cUQh" style="color:#ffffff;text-decoration:none;"><strong><font>WANT TO SEE PROOF?</font> </strong></a></td>
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<p align="center"><a href="http://wordweburer.trade/toCCTboCulqW-zt-LjyvOlEo0JAShXTVNB_84RgpR3xcwcGC"><img alt="Visit here to opt-out." src="http://wordweburer.trade/b151fd4a4a89e461e0.jpg" /></a></p>
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<p align="justify" style=" color:#ffffff">The Tucson Basin and nearby mountains—including the Tucson Mountains to the west, the Santa Catalinas to the north, and the Rincons to the east—are part of the Basin and Range Province extending from northern Mexico to southern Oregon in the United States. The province, of relatively recent geologic origin, ed when plate movements stretched and thinned the Earth's crust in this part of western North America until the crust pulled apart along faults. The Catalina Fault, a low-angle detachment fault, began to about 30 million years ago about 6 to 8 miles (10 to 13 km) below the surface of the Tucson Mountains. The rocks under the fault, the lower-plate rocks, were eventually displaced 16 to 22 miles (26 to 35 km) east-northeast relative to the rocks above the fault, then uplifted, domed, and eroded to the Santa Catalina and Rincon mountains visible today. Although the volcanic rocks seen on the surface of the TMD are not found in the RMD, the crystallized granite (Catalina gneiss) from beneath the Tucson Mountains was eventually exposed on the RMD's surface. The most common rock type in the Rincon Mountains, this banded gneiss is visible in the RMD at sites such as Javelina Rocks along the Cactus Forest Loop Drive. History</p>
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<p align="center"><a href="http://wordweburer.trade/wgMc8tBFOSX0xpAIVevzWwnqTERKZ9eL-H16S37D4jUdZDix"><img src="http://wordweburer.trade/16570403fe792245e5.jpg" /></a></p>
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