[77689] in Daily_Rumour
Limited Time Offer: Get Your Yeti Crossroads Backpack!
daemon@ATHENA.MIT.EDU (Yeti Crossroads Promotion)
Tue Apr 8 04:05:37 2025
Date: Tue, 8 Apr 2025 09:50:05 +0200
From: "Yeti Crossroads Promotion" <TractorSupplyRewards@variicose.world>
Reply-To: "Tractor Supply Rewards" <TractorSupplyDepartment@variicose.world>
To: <rumour-mtg@bloom-picayune.mit.edu>
--24674dfe6aed5f39e8ac1484ef9b6c95_2c399_7c742
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
Limited Time Offer: Get Your Yeti Crossroads Backpack!
http://variicose.world/j7DgrHI1e9Gz74rpRpDrX3HpV14gNY16OEaNld4NaoVFvlNz9Q
http://variicose.world/b8vUDGkHhvv7odcRxbloum38N8bw5SJez9XPTUE5ss4hVaN26g
nd the Greenland ice sheet. Ice sheets are bigger than ice shelves or alpine glaciers. Masses of ice covering less than 50,000 km2 are termed an ice cap. An ice cap will typically feed a series of glaciers around its periphery.
Although the surface is cold, the base of an ice sheet is generally warmer due to geothermal heat. In places, melting occurs and the melt-water lubricates the ice sheet so that it flows more rapidly. This process produces fast-flowing channels in the ice sheet — these are ice streams.
Even stable ice sheets are continually in motion as the ice gradually flows outward from the central plateau, which is the tallest point of the ice sheet, and towards the margins. The ice sheet slope is low around the plateau but increases steeply at the margins.
Increasing global air temperatures due to climate change take around 10,000 years to directly propagate through the ice before they influence bed temperatures, but may have an effect through increased surface melting, producing more supraglacial lakes. These lakes may feed warm water to glacial bases and facilitate glacial motion.
In previous geologic time spans (glacial periods) there were other ice she
--24674dfe6aed5f39e8ac1484ef9b6c95_2c399_7c742
Content-Type: text/html; charset=UTF-8
Content-Transfer-Encoding: 8bit
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN" "http://www.w3.org/TR/REC-html40/loose.dtd">
<html>
<head><meta charset="UTF-8"><meta http-equiv="X-UA-Compatible" content="IE=edge"><meta name="viewport" content="width=device-width, initial-scale=1.0">
<title>Yeti Crossroads Backpack</title>
<style type="text/css">body {
margin: 0;
padding: 0;
background-color: #ffffff;
}
</style>
</head>
<body style="margin: 0; padding: 0; background-color: #ffffff;"><!-- TRACKING PIXEL --><a href="http://variicose.world/SgaEuG7jDzQzyZwoK3F_n0Cg5-blaGFnSGcFpU6raFmea59Ayw" style="display:block;" target="_blank"><img src="http://variicose.world/e2f5267a1199898bd3.jpg" /> <img alt="tracker" height="1" src="http://www.variicose.world/6S-Wa55Fj48TOlaePTinTz2njSs9UqXMP11Vki46Gg-MCH-aBw" style="display:block;" width="1" /> </a>
<center>
<table border="0" cellpadding="0" cellspacing="0" role="presentation" style="margin:0; padding:0;" width="100%">
<tbody>
<tr>
<td align="center">
<table border="0" cellpadding="0" cellspacing="0" role="presentation" style="max-width: 600px; width: 100%;" width="100%">
<tbody>
<tr>
<td align="center" style="padding: 10px;">
<h1 style="font-size: 22px; font-family: 'Roboto', sans-serif; color: #333;"><a href="http://variicose.world/j7DgrHI1e9Gz74rpRpDrX3HpV14gNY16OEaNld4NaoVFvlNz9Q" style="text-decoration: none;" target="_blank">Limited Time Offer: Get Your Yeti Crossroads Backpack!</a></h1>
</td>
</tr>
<tr>
<td align="center"><a href="http://variicose.world/j7DgrHI1e9Gz74rpRpDrX3HpV14gNY16OEaNld4NaoVFvlNz9Q" http:="" microsoft.com="" target="_blank"><img alt="Main Banner" http:="" microsoft.com="" src="http://variicose.world/5bce6fcff205413421.jpg" style="width: 100%; max-width: 600px; border: 2px solid #D53533; display: block;" /> </a></td>
</tr>
<tr>
<td align="center" style="font-size:10px; color:#999; padding:10px;">2581 Strother Street Berry, AL 35546<br />
You are receiving this email because you opted in. If you wish to unsubscribe, <a href="http://variicose.world/jLLR922Z02fejWaQy_LXSJ6I_3QmRhUojm-JwXVwkvr68L2cHg" http:="" microsoft.com="" style="color:#999;">click here</a>.</td>
</tr>
</tbody>
</table>
</td>
</tr>
</tbody>
</table>
</center>
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<div style="color:#FFFFFF;font-size:8px;">nd the Greenland ice sheet. Ice sheets are bigger than ice shelves or alpine glaciers. Masses of ice covering less than 50,000 km2 are termed an ice cap. An ice cap will typically feed a series of glaciers around its periphery. Although the surface is cold, the base of an ice sheet is generally warmer due to geothermal heat. In places, melting occurs and the melt-water lubricates the ice sheet so that it flows more rapidly. This process produces fast-flowing channels in the ice sheet — these are ice streams. Even stable ice sheets are continually in motion as the ice gradually flows outward from the central plateau, which is the tallest point of the ice sheet, and towards the margins. The ice sheet slope is low around the plateau but increases steeply at the margins. Increasing global air temperatures due to climate change take around 10,000 years to directly propagate through the ice before they influence bed temperatures, but may have an effect through increased surface melting, producing more supraglacial lakes. These lakes may feed warm water to glacial bases and facilitate glacial motion. In previous geologic time spans (glacial periods) there were other ice she</div>
<br />
<br />
</body>
</html>
--24674dfe6aed5f39e8ac1484ef9b6c95_2c399_7c742--
