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Envelope-to: b.smith@smithfamilycarpets.com
Delivery-date: Sat, 17 Apr 2021 05:28:30 -0500
To: <b.smith@smithfamilycarpets.com>
Date: Sat, 17 Apr 2021 03:27:25 -0700
Message-ID: <2410387481443542410106812816192309@gqfyyt.nohurt.us>
From: "Constipation Gone" <ConstipationGone@nohurt.us>
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Subject:    Your gut has 17lbs of rotting food bloating it

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Is your belly bigger than you’d like? If so, 17 pounds of undigested food may be rotting in your digestive system, but doctors recently discovered a new molecule that helps get rid of it when you do this for 10 seconds after brushing your teeth.

Imagine 17 pounds gone with ZERO change in diet or exercise.
http://www.nohurt.us/2410-128-1068-48144354/b.smith/tindex7.html
Imagine shrinking a big tummy in 24 hours.

It’s not just possible, it’s easy when this new patented molecule flips your “slim gut switch.”

Here’s how to do it…

==> Your gut has 17lbs of rotting food bloating it
http://www.nohurt.us/2410-128-1068-48144354/b.smith/tindex8.html





 
c volcanism inside the crater Lowell,[82][83] Orientale basin, located in the transition zone between the near and far sides of the Moon. An initially hotter mantle and/or local enrichment of heat-producing elements in the mantle could be responsible for prolonged activities also on the far side in the Orientale basin.[84][85] The lighter-colored regions of the Moon are called terrae, or more commonly highlands, because they are higher than most maria. They have been radiometrically dated to having formed 4.4 billion years ago, and may represent plagioclase cumulates of the lunar magma ocean.[75][76] In contrast to Earth, no major lunar mountains are believed to have formed as a result of tectonic events.[86] The concentration of maria on the Near Side likely reflects the substantially thicker crust of the highlands of the Far Side, which may have formed in a slow-velocity impact of a second moon of Earth a few tens of millions of years after their formation.[87][88] Impact craters Further information: List of craters on the Moon A gray, many-ridged surface from high above. The largest feature is a circular ringed structure with high walled sides and a lower central peak: the entire surface out to the horizon is filled with similar structures that are smaller and overlapping. Lunar crater Daedalus on the Moon's far side The other major geologic process that has affected the Moon's surface is impact cratering,[89] with craters formed when asteroids and comets collide with the lunar surface. There are estimated to be roughly 300,000 craters wider than 1 km (0.6 mi) on the Moon's near side alone.[90] The lunar geologic timescale is based on the most prominent impact events, including Nectaris, Imbrium, and Orientale, structures characterized by multiple rings of uplifted material, between hundreds and thousands of kilometers in diameter and associated with a broad apron of ejecta deposits that form a regional stratigraphic horizon.[91] The lack of an atmosphere, weather and recent geological processes mean that many of these craters are well-preserved. Although only a few multi-ring basins have been definitively dated, they are useful for assigning relative ages. Because impact craters ac





http://www.nohurt.us/2410-128-1068-48144354/b.smith/tindex9.html










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