From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest)
To: ammf-digest@smoe.org
Subject: alt.music.moxy-fruvous digest V14 #8985
Reply-To: ammf@fruvous.com
Sender: owner-ammf-digest@smoe.org
Errors-To: owner-ammf-digest@smoe.org
Precedence: bulk


alt.music.moxy-fruvous digest Saturday, May 21 2022 Volume 14 : Number 8985



                               Today's Subjects:
                               -----------------
  You have absolutely nothing to lose!  ["100% Satisfaction Guarantee" <100S]

----------------------------------------------------------------------

Date: Sat, 21 May 2022 15:07:51 -0400
From: "100% Satisfaction Guarantee" <100SatisfactionGuarantee@easyflexor.buzz>
Subject: You have absolutely nothing to lose!

You have absolutely nothing to lose!

http://easyflexor.buzz/bBgXi3ROaADWP-t4NbHNGzVV658oHcTPJ2la1hore8xMIajbjA

http://easyflexor.buzz/5DDiwsBORhG6Fripd2cn1uYPcDO_bNXwbsKEjGhP4nlgM7Ma

irrocumulus clouds form in sheets or patches and do not cast shadows. They commonly appear in regular, rippling patterns or in rows of clouds with clear areas between. Cirrocumulus are, like other members of the cumuliform category, formed via convective processes. Significant growth of these patches indicates high-altitude instability and can signal the approach of poorer weather. The ice crystals in the bottoms of cirrocumulus clouds tend to be in the form of hexagonal cylinders. They are not solid, but instead tend to have stepped funnels coming in from the ends. Towards the top of the cloud, these crystals have a tendency to clump together. These clouds do not last long, and they tend to change into cirrus because as the water vapor continues to deposit on the ice crystals, they eventually begin to fall, destroying the upward convection. The

------------------------------

End of alt.music.moxy-fruvous digest V14 #8985
**********************************************