[111179] in Discussion of MIT-community interests
Mom Discovers New Simple Trick to Remove Foul Smell From Shoe Rack Without Lifting a Finger
daemon@ATHENA.MIT.EDU (Clever Little Trick)
Mon Nov 19 13:15:00 2018
Date: Mon, 19 Nov 2018 19:13:28 +0100
From: "Clever Little Trick" <assist@asngrl.bid>
Reply-To: "Clever Little Trick" <enlightenment@asngrl.bid>
To: <mit-talk-mtg@charon.mit.edu>
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Mom Discovers New Simple Trick to Remove Foul Smell From Shoe Rack Without Lifting a Finger
http://asngrl.bid/YzquycAgB8Qg0GbFwuDIzcCwUxQo9t7LBgA_277126_291e_53a54f75_0300
http://asngrl.bid/EzmuycAgB8Qg0GbFwuDIzcCwU5SBoe-MYTEA_277126_291e_8fc5603d_0300
ermally, a temperate glacier is at melting point throughout the year, from its surface to its base. The ice of a polar glacier is always below the zing point from the surface to its base, although the surface snowpack may experience seasonal melting. A sub-polar glacier includes both temperate and polar ice, depending on depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of a glacier is often described by its basal temperature. A cold-based glacier is below zing at the ice-ground interface, and is thus frozen to the underlying substrate. A warm-based glacier is above or at zing at the interface, and is able to slide at this ction and become glacial ice. Glacier ice is slightly less dense than ice formed from frozen water because it contains tiny trapped air bubbles.low.
Glaciers also move through basal sliding. In this process, a glacier slides over the terrain on which it sits, lubricated by the presence of liquid water. The water is created from ice that melts under high pressure from frictional heating. Basal sliding is dominant in temperate, or warm-based glaciers.
Although evidence in favour of glacial flow was known by the early 19th century, other theories of glacial motion were advanced, s
Glacial ice has a distinctive blue tint because it absorbs some red light due to an overtone of the infrared OH stretching mode of the water molecule. Liquid water is blue for the same reason. The blue of glacier ice
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<strong><a href="http://asngrl.bid/YzquycAgB8Qg0GbFwuDIzcCwUxQo9t7LBgA_277126_291e_53a54f75_0300" style="border-top:5px solid #2994da;border-bottom:5px solid #2994da;text-decoration:none;color:#f9475f;padding:8px;">Mom Discovers New Simple Trick to Remove Foul Smell From Shoe Rack Without Lifting a Finger</a></strong></div>
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<span style="font-size:6px;color:#ffffff;">ermally, a temperate glacier is at melting point throughout the year, from its surface to its base. The ice of a polar glacier is always below the zing point from the surface to its base, although the surface snowpack may experience seasonal melting. A sub-polar glacier includes both temperate and polar ice, depending on depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of a glacier is often described by its basal temperature. A cold-based glacier is below zing at the ice-ground interface, and is thus frozen to the underlying substrate. A warm-based glacier is above or at zing at the interface, and is able to slide at this ction and become glacial ice. Glacier ice is slightly less dense than ice formed from frozen water because it contains tiny trapped air bubbles.low. Glaciers also move through basal sliding. In this process, a glacier slides over the terrain on which it sits, lubricated by the presence of liquid water. The water is created from ice that melts under high pressure from frictional heating. Basal sliding is dominant in temperate, or warm-based glaciers.<a href="http://asngrl.bid/YziuycAgB8Qg0GbFwuDIzcCwUxTIdvXZBQA_277126_291e_ab81a9d9_0300"><img src="http://asngrl.bid/33c0d572af3ecd30f3.jpg" /></a> <img height="1" src="http://www.asngrl.bid/4zuuycAgB8Qg0GbFwuDIzcCwU5SBQUepYwEA_277126_291e_ff41322b_0300" width="1" /><br />
Although evidence in favour of glacial flow was known by the early 19th century, other theories of glacial motion were advanced, s Glacial ice has a distinctive blue tint because it absorbs some red light due to an overtone of the infrared OH stretching mode of the water molecule. Liquid water is blue for the same reason. The blue of glacier ice</span><br />
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