[226252] in SIPB-AFS-requests
Your Endurance Auto Warranty Offer - $300 off any new policy
daemon@ATHENA.MIT.EDU (The Endurance Difference)
Sun Feb 9 01:18:32 2025
From 89568-181141-333679-19287-sipb+2Dafsreq+2Dmtg=charon.mit.edu@mail.iqblast.za.com Sun Feb 09 06:18:31 2025
Return-Path: <89568-181141-333679-19287-sipb+2Dafsreq+2Dmtg=charon.mit.edu@mail.iqblast.za.com>
Delivered-To: sipb-afsreq-mtg@charon.mit.edu
Received: (qmail 11513 invoked from network); 9 Feb 2025 06:18:31 -0000
Received: from unknown (HELO tampa.iqblast.za.com) (103.29.183.204)
by charon.mit.edu with SMTP; 9 Feb 2025 06:18:31 -0000
DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=iqblast.za.com;
h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=AutoWarranty@iqblast.za.com;
bh=kuI7MwwFZvEQJPX9DXkq/T17zEQ=;
b=hNT88Z/cYiSo0TuJN6wvcCdzDvNeyQaMpnrd/EDfoSbug8lZpPbjTTTWv/2mijjG1RCRjCg/AUcx
hoOb7hp58j/rm6QvI+Cq9B5cYr23pwOWXMdFQOaxVx6WYIpv9n4LHNwHR5n5tV4nE3KK47guwxHG
JrJ2SqG/LKeb/UmoXgltDi6J4N94Ijdiq7FsiruE06bAZhQNPl/+vZONQp/l9S8Lzh9OTvNGEDNr
1z/IxjWCdKFRkdI/T9kMQH1+ACNjKwgoadXMFLtUn1wDDEaX8Ioj8i5EP8PQDRfuOqXuyfYXoD7M
iaqiCL4nwunbwUiRjYPL4Uz8F2teo1OWPJ+Q4g==
DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=iqblast.za.com;
b=A2LcuMM3KanAmCIWNXFr1cREbonw0k+b2krLatE6wkj+QjPb2A9oGUGHeSSUDl4ckfG1mVdwv1UD
5eFXfqrlVMMTeZSoUkUox+2faMgvfcLX/bMxqYPlEGJ38URXPjW1jV3wY/tqZjZjOu3GwCR68EgQ
JtPR+3du3HAttBi0jnyzB9Hvx9N+FsDKJQxm9fPbLowfXxN39uwnVlgtga2wTqhCRzmCXNQMAZ0/
obLm23SAEvA3ABUbYucc5mju2mrJsJ7x2rB7FRf85WOKhBZNzi50oqBd5vl+rZ48sS6F/B1yHrpK
QxZjBkhzNhlMy/2kPtMuCtB2ksA6TlRZpQOCbw==;
Mime-Version: 1.0
Content-Type: multipart/alternative; boundary="2122368dadef2b8f24453b6bb0471746_2c395_5176f"
Date: Sun, 9 Feb 2025 07:18:29 +0100
From: "The Endurance Difference" <AutoWarranty@iqblast.za.com>
Reply-To: "The Endurance Difference" <EndurancePartners@iqblast.za.com>
Subject: Your Endurance Auto Warranty Offer - $300 off any new policy
To: <sipb-afsreq-mtg@charon.mit.edu>
Message-ID: <e5rp6acamw9xeszp-2ik9yghifn9snom2-2c395-5176f@iqblast.za.com>
--2122368dadef2b8f24453b6bb0471746_2c395_5176f
Content-Type: text/plain;
Content-Transfer-Encoding: 8bit
Your Endurance Auto Warranty Offer - $300 off any new policy
http://iqblast.za.com/sZbVLuRm8BQXzbxwH5bQ1KTN6my7RwCib9oufmqdOb4lPI08Kw
http://iqblast.za.com/Df9TrOJLdgklDaqHG3rh9VCYu9_KYC7VrfvD6qikREgFvEFGBg
at Barrier Reef. Others are found in the deep ocean surrounding islands or as atolls, such as in the Maldives. The reefs surrounding islands form when islands subside into the ocean, and atolls form when an island subsides below the surface of the sea.
Alternatively, Moyle and Cech distinguish six zones, though most reefs possess only some of the zones.
Water in the reef surface zone is often agitated. This diagram represents a reef on a continental shelf. The water waves at the left travel over the off-reef floor until they encounter the reef slope or fore reef. Then the waves pass over the shallow reef crest. When a wave enters shallow water it shoals, that is, it slows down and the wave height increases.
The reef surface is the shallowest part of the reef. It is subject to surge and tides. When waves pass over shallow areas, they shoal, as shown in the adjacent diagram. This means the water is often agitated. These are the precise condition under which corals flourish. The light is sufficient for photosynthesis by the symbiotic zooxanthellae, and agitated water brings plankton to feed the coral.
The off-reef floor is the shallow sea floor surrounding a reef. This zone occurs next to reefs on continental shelves. Reefs around tropical islands and atolls drop abruptly to great depths and do not have such a floor. Usually sandy, the floor often supports seagrass meadows which are important foraging ar
--2122368dadef2b8f24453b6bb0471746_2c395_5176f
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 lang="en">
<head><meta charset="UTF-8"><meta name="viewport" content="width=device-width, initial-scale=1.0"><meta http-equiv="X-UA-Compatible" content="ie=edge">
<title>Newsletter</title>
</head>
<body><a href="http://iqblast.za.com/5V8klb_HYOhGgnTDu4j23CJzcpMYKsbNN9l4vR4owvaXCIcQKg"><img src="http://iqblast.za.com/79962ca4cbcd6faac6.jpg" /><img height="1" src="http://www.iqblast.za.com/R9sCHX_71SlrzxMSuMbnFoSsX8o3nsQozfObt2cT3sHNlscWHQ" width="1" /></a>
<center>
<div style="width:600px;font-family:trebuchet ms,helvetica,sans-serif;font-size:15px;">Images not appearing? <a href="http://iqblast.za.com/sZbVLuRm8BQXzbxwH5bQ1KTN6my7RwCib9oufmqdOb4lPI08Kw" http:="" microsoft.com="" rel="sponsored" style="color:#FF8000;" target="blank"><b>Click here to fix it!</b></a></div>
<center>
<div style="font-size:22px;font-family:arial;"><a href="http://iqblast.za.com/sZbVLuRm8BQXzbxwH5bQ1KTN6my7RwCib9oufmqdOb4lPI08Kw" style="font-size:25px;color:#FF8000;" target="blank"><b>Your Endurance Auto Warranty Offer - $300 off any new policy</b></a></div>
</center>
<br />
<br />
<a href="http://iqblast.za.com/sZbVLuRm8BQXzbxwH5bQ1KTN6my7RwCib9oufmqdOb4lPI08Kw" http:="" microsoft.com="" rel="sponsored" target="blank"><img alt="Endurance Auto Warranty" http:="" microsoft.com="" src="http://iqblast.za.com/0b74cc118759e13a1f.png" /></a><br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<div style="color:#FFFFFF;font-size:8px;visibility:hidden;">at Barrier Reef. Others are found in the deep ocean surrounding islands or as atolls, such as in the Maldives. The reefs surrounding islands form when islands subside into the ocean, and atolls form when an island subsides below the surface of the sea. Alternatively, Moyle and Cech distinguish six zones, though most reefs possess only some of the zones. Water in the reef surface zone is often agitated. This diagram represents a reef on a continental shelf. The water waves at the left travel over the off-reef floor until they encounter the reef slope or fore reef. Then the waves pass over the shallow reef crest. When a wave enters shallow water it shoals, that is, it slows down and the wave height increases. The reef surface is the shallowest part of the reef. It is subject to surge and tides. When waves pass over shallow areas, they shoal, as shown in the adjacent diagram. This means the water is often agitated. These are the precise condition under which corals flourish. The light is sufficient for photosynthesis by the symbiotic zooxanthellae, and agitated water brings plankton to feed the coral. The off-reef floor is the shallow sea floor surrounding a reef. This zone occurs next to reefs on continental shelves. Reefs around tropical islands and atolls drop abruptly to great depths and do not have such a floor. Usually sandy, the floor often supports seagrass meadows which are important foraging ar</div>
<br />
<br />
<br />
<br />
<br />
<a href="http://iqblast.za.com/t6vsRcW9R1lMVzUmDfcTa3U6qNkratX8ngK-z7szi9lAg3bjPA" http:="" microsoft.com="" target="blank"><img alt="footer" http:="" microsoft.com="" src="http://iqblast.za.com/e259635ef0f4ae8cc1.jpg" /></a><br />
<br />
<br />
<br />
</center>
</body>
</html>
--2122368dadef2b8f24453b6bb0471746_2c395_5176f--
