Return-path: <60968-93744-396881-12934-llg+2Dboard=lojban.org@mail.deltaairline.today> Envelope-to: llg-board@lojban.org Delivery-date: Wed, 01 Feb 2023 23:29:32 -0800 Received: from [62.197.136.174] (port=44926 helo=lowell.deltaairline.today) by d7893716a6e6 with esmtp (Exim 4.94.2) (envelope-from <60968-93744-396881-12934-llg+2Dboard=lojban.org@mail.deltaairline.today>) id 1pNU2D-0026Fe-HY for llg-board@lojban.org; Wed, 01 Feb 2023 23:29:31 -0800 DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=deltaairline.today; h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=TargetShopperGiftCardChance@deltaairline.today; bh=V/U2lWYM+vJ/+i/7OHqXwTQtmo0=; b=P8J1CgdEkM+GFmSAftWk0xr0Y96F67X5xr0aQrf2hvNvZ+GRNCdDvypkkSzwSP2G4l/kKbP4G1/Y +vme5wxlYeraXGghEaoj5o6x000lSAAGTB/NgQGMFCoAu90hmEUKDkA4CKsrcR2gW2ywUFyF5cwi aRIxJhgCkYHwTD8N2PQ= DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=deltaairline.today; b=lGmFHdaSCThxc5BtANOLaaw1xU5R/uMlU5xd5B4PAbGXuqCPWDJjhmkZv9AhFK4tXk5TNuT7jkEG bCX4u9j1dhV7lZD1TJBiz3QV1lVYBAC7U4rTVg872MoV6sdvxIjC0wxGlLsRsl8t8+HI9bFitIWR Aw3JL3OgQwBfU8U7634=; Mime-Version: 1.0 Content-Type: multipart/alternative; boundary="a5132a97c6405fec300aef9029f65cbf_16e30_60e51" Date: Thu, 2 Feb 2023 08:29:26 +0100 From: "Target Shopper Feedback" Reply-To: "Target Shopper Feedback" Subject: Congratulations! You can get a $50 Target gift card! To: Message-ID: X-Spam-Score: -1.9 (-) X-Spam_score: -1.9 X-Spam_score_int: -18 X-Spam_bar: - --a5132a97c6405fec300aef9029f65cbf_16e30_60e51 Content-Type: text/plain; Content-Transfer-Encoding: 8bit Congratulations! You can get a $50 Target gift card! http://deltaairline.today/k8442-HjazDs0yR_K4hHzuKt2en1SawNjgvCJNUg12IkThyonQ http://deltaairline.today/94CQIUfXv8gSCS0aLiXuDbPqrfgYa5UJcN-NN7cTh3eDHhLK Resolution Guyot is part of the western Mid-Pacific Mountains, located west of Hawaii, north-northeast of the Marshall Islands. Unlike conventional Pacific Ocean island chains, the Mid-Pacific Mountains are a group of oceanic plateaus with guyots (also known as tablemounts)) that become progressively younger towards the east. Other guyots in the Mid-Pacific Mountains are Sio South, Darwin, Thomas, Heezen, Allen, Caprina, Jacqueline and Allison. The seamount is about 500 metres (1,600 ft) high and rises from a raised seafloor to a depth of about 1,320 metres (4,330 ft). At a depth of 1,300–1,400 metres (4,300–4,600 ft) it is capped off by a 25 by 35 kilometres (16 mi × 22 mi) wide rather flat and roughly circular summit platform with a 25 metres (82 ft) high rim and a moat inside of this rim. At the margin of the platform, structures interpreted as sea cliffs or wave cut terraces have been found; at one site there is a terrace about 200 metres (660 ft) wide, surmounted by a 25 metres (82 ft) high cliff. Pinnacles and depressions dot the surface platform. The surface of the platform consists of limestone that is partially covered by pelagic sediments; underwater cameras have shown the presence of rock slabs covered by ferromanganese crusts. The guyot rises from a seafloor of Jurassic age (201.3 ± 0.2 – ca. 145 million years ago) that might be as much as 154 million years old. Terrestrial organic material on the seafloor around Resolution Guyot originated from when it was still an island, and carbonate sediments swept away from the guyot ended up on the surrounding seaflo --a5132a97c6405fec300aef9029f65cbf_16e30_60e51 Content-Type: text/html; Content-Transfer-Encoding: 8bit Newsletter

Congratulations! You can get a $50 Target gift card!











Resolution Guyot is part of the western Mid-Pacific Mountains, located west of Hawaii, north-northeast of the Marshall Islands. Unlike conventional Pacific Ocean island chains, the Mid-Pacific Mountains are a group of oceanic plateaus with guyots (also known as tablemounts)) that become progressively younger towards the east. Other guyots in the Mid-Pacific Mountains are Sio South, Darwin, Thomas, Heezen, Allen, Caprina, Jacqueline and Allison. The seamount is about 500 metres (1,600 ft) high and rises from a raised seafloor to a depth of about 1,320 metres (4,330 ft). At a depth of 1,300–1,400 metres (4,300–4,600 ft) it is capped off by a 25 by 35 kilometres (16 mi × 22 mi) wide rather flat and roughly circular summit platform with a 25 metres (82 ft) high rim and a moat inside of this rim. At the margin of the platform, structures interpreted as sea cliffs or wave cut terraces have been found; at one site there is a terrace about 200 metres (660 ft) wide, surmounted by a 25 metres (82 ft) high cliff. Pinnacles and depressions dot the surface platform. The surface of the platform consists of limestone that is partially covered by pelagic sediments; underwater cameras have shown the presence of rock slabs covered by ferromanganese crusts. The guyot rises from a seafloor of Jurassic age (201.3 ± 0.2 – ca. 145 million years ago) that might be as much as 154 million years old. Terrestrial organic material on the seafloor around Resolution Guyot originated from when it was still an island, and carbonate sediments swept away from the guyot ended up on the surrounding seaflo














 
--a5132a97c6405fec300aef9029f65cbf_16e30_60e51--