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To: <b.smith@smithfamilycarpets.com>
Date: Thu, 13 Jan 2022 03:55:59 -0800
From: "Comfy Corset" <ComfyCorset@activatorz.us>
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Subject:    Comfy Corset™ Doesn't Constrict or Squeeze

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In the 1960s, it was discovered that the Earth's lithosphere, which includes the crust and rigid uppermost portion of the upper mantle, is separated into tectonic plates that move across the plastically deforming, solid, upper mantle, which is called the asthenosphere. This theory is supported by several types of observations, including seafloor spreading[6][7] and the global distribution of mountain terrain and seismicity. There is an intimate coupling between the movement of the plates on the surface and the convection of the mantle (that is, the heat transfer caused by the bulk movement of molecules within fluids). Thus, oceanic plates and the adjoining mantle convection currents always move in the same direction – because the oceanic lithosphere is actually the rigid upper thermal boundary layer of the convecting mantle. This coupling between rigid plates moving on the surface of the Earth and the convecting mantle is called plate tectonics. In this diagram based on seismic tomography, subducting slabs are in blue and continental margins and a few plate boundaries are in red. The blue blob in the cutaway section is the Farallon Plate, which is subducting beneath North America. The remnants of this plate on the surface of the Earth are the Juan de Fuca Plate and Explorer Plate, both in the northwestern United States and southwestern Canada and the Cocos Plate on the west coast of Mexico. The development of plate tectonics has provided a physical basis for many observations of the solid Earth. Long linear regions of geological features are explained as plate boundaries.[8] For example: Mid-ocean ridges, high regions on the seafloor where hydrothermal vents and volcanoes exist, are seen as divergent boundaries, where two plates move apart. Arcs of volcanoes and earthquakes are theorized as convergent boundaries, where one plate subducts, or moves, under anoth



















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=09<tbody>
=09=09<tr>
=09=09=09<td style=3D"display:none !important; visibility:hidden; mso-hide:=
all; font-size:1px; color:#ffffff; line-height:1px; max-height:0px; max-wid=
th:0px; opacity:0; overflow:hidden;">Custom Fits Your Breast Shape & Size A=
nd Adjusts Side To Side For A Balanced Look!</td>
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8px;">Comfy Corset&trade; Bra &mdash; Comfy As A Cami But Sexy As A Corset<=
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=09=09=09<p style=3D"font:12px Arial, Helvetica, sans-serif; line-height: 1=
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ry front cross-band design easily adjusts the bands over and under. No more=
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=09=09=09<p style=3D"font:12px Arial, Helvetica, sans-serif; line-height: 1=
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=09=09=09<td align=3D"center">
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<a href=3D"http://www.activatorz.us/l/lc3R6521G82WL/3190JC5536AH6827L117IJ4=
8144354PT1566796052" http://microsoft.com/**0drZpCmfJwjcNvm** rel=3D"sponso=
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&nbsp;<br />
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<p style=3D"color:#FFFFFF;font-size:5px;">In the 1960s, it was discovered t=
hat the Earth's lithosphere, which includes the crust and rigid uppermost p=
ortion of the upper mantle, is separated into tectonic plates that move acr=
oss the plastically deforming, solid, upper mantle, which is called the ast=
henosphere. This theory is supported by several types of observations, incl=
uding seafloor spreading[6][7] and the global distribution of mountain terr=
ain and seismicity.

There is an intimate coupling between the movement of the plates on the sur=
face and the convection of the mantle (that is, the heat transfer caused by=
 the bulk movement of molecules within fluids). Thus, oceanic plates and th=
e adjoining mantle convection currents always move in the same direction =
=E2=80=93 because the oceanic lithosphere is actually the rigid upper therm=
al boundary layer of the convecting mantle. This coupling between rigid pla=
tes moving on the surface of the Earth and the convecting mantle is called =
plate tectonics.


In this diagram based on seismic tomography, subducting slabs are in blue a=
nd continental margins and a few plate boundaries are in red. The blue blob=
 in the cutaway section is the Farallon Plate, which is subducting beneath =
North America. The remnants of this plate on the surface of the Earth are t=
he Juan de Fuca Plate and Explorer Plate, both in the northwestern United S=
tates and southwestern Canada and the Cocos Plate on the west coast of Mexi=
co.
The development of plate tectonics has provided a physical basis for many o=
bservations of the solid Earth. Long linear regions of geological features =
are explained as plate boundaries.[8]

For example:

Mid-ocean ridges, high regions on the seafloor where hydrothermal vents and=
 volcanoes exist, are seen as divergent boundaries, where two plates move a=
part.
Arcs of volcanoes and earthquakes are theorized as convergent boundaries, w=
here one plate subducts, or moves, under anoth</p>
<br />
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<br />
<br />
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<br />
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<a href=3D"http://www.activatorz.us/unsD6521T82EF/3190I5536V6827N117IK48144=
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=09=09=09</td>
=09=09</tr>
=09</tbody>
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