Return-path: <60987-93744-396881-13051-llg+2Dboard=lojban.org@mail.savagegrowpluszy.today> Envelope-to: llg-board@lojban.org Delivery-date: Thu, 02 Feb 2023 03:40:18 -0800 Received: from [62.197.136.175] (port=47309 helo=aoede.savagegrowpluszy.today) by d7893716a6e6 with esmtp (Exim 4.94.2) (envelope-from <60987-93744-396881-13051-llg+2Dboard=lojban.org@mail.savagegrowpluszy.today>) id 1pNXwu-0027Ac-9P for llg-board@lojban.org; Thu, 02 Feb 2023 03:40:17 -0800 DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=savagegrowpluszy.today; h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=Translator@savagegrowpluszy.today; bh=ztQDhNVIQZFlwd/aRwHQ0R7w/fk=; b=Gw8D1Su4/LbZtUWpwhQzp+lbIHnaWdM/cUoZViAKiUhXZncKtDSeKBN+L4QFh9wE0ZcZSfD0Zl09 YkpO14iFXOoJPLc0myYUyXzNIqRYicJU7+uI+ItlrUB/d05ppp9JNZ/bWE5SKsgRBG84zftV9yDy 53DU+EWT/9b8c+t48EQ= DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=savagegrowpluszy.today; b=NUKmuGe5fcJGMwR893PORE1RVMe9bgCqJe/MkerKlXjfWg4des+Qxj4NKBqcZpbcRZvZ0rTgcaHK 3WTUK9PaPhUyOscFSIIMA3CVVpTIgl82DXsriqIJSgdAuvCPFaIYrhQlGb05Yq4eLjUpHfQj91Nj vaL7V6bYXgocFk5gQfc=; Mime-Version: 1.0 Content-Type: multipart/alternative; boundary="550dd8586b4db0d1699ab199eea250cc_16e30_60e51" Date: Thu, 2 Feb 2023 11:52:48 +0100 From: "Translator" Reply-To: "Translator" Subject: Order Now To Get A Special 5O% OFF To: Message-ID: X-Spam-Score: 4.9 (++++) X-Spam_score: 4.9 X-Spam_score_int: 49 X-Spam_bar: ++++ X-Spam-Report: Spam detection software, running on the system "f6db9eef8881", has NOT identified this incoming email as spam. The original message has been attached to this so you can view it or label similar future email. If you have any questions, see @@CONTACT_ADDRESS@@ for details. Content preview: Order Now To Get A Special 5O% OFF http://savagegrowpluszy.today/M4PHCRll5MeIrJJmmPFkKESPfY-0932eLGEz9q4Kyd1up3BmuQ http://savagegrowpluszy.today/tG1Kq7dXa32RnPXibXd2yJdhmoRZu91GFT40f9Duk0TljnqrUw Content analysis details: (4.9 points, 5.0 required) pts rule name description ---- ---------------------- -------------------------------------------------- 0.8 BAYES_50 BODY: Bayes spam probability is 40 to 60% [score: 0.5000] 0.0 URIBL_BLOCKED ADMINISTRATOR NOTICE: The query to URIBL was blocked. See http://wiki.apache.org/spamassassin/DnsBlocklists#dnsbl-block for more information. [URIs: savagegrowpluszy.today] 0.0 URIBL_DBL_BLOCKED_OPENDNS ADMINISTRATOR NOTICE: The query to dbl.spamhaus.org was blocked due to usage of an open resolver. See https://www.spamhaus.org/returnc/pub/ [URIs: savagegrowpluszy.today] 1.3 RCVD_IN_BL_SPAMCOP_NET RBL: Received via a relay in bl.spamcop.net [Blocked - see ] 0.0 RCVD_IN_ZEN_BLOCKED_OPENDNS RBL: ADMINISTRATOR NOTICE: The query to zen.spamhaus.org was blocked due to usage of an open resolver. See https://www.spamhaus.org/returnc/pub/ [62.197.136.175 listed in zen.spamhaus.org] -5.0 RCVD_IN_DNSWL_HI RBL: Sender listed at https://www.dnswl.org/, high trust [62.197.136.175 listed in list.dnswl.org] 0.0 URIBL_ZEN_BLOCKED_OPENDNS ADMINISTRATOR NOTICE: The query to zen.spamhaus.org was blocked due to usage of an open resolver. See https://www.spamhaus.org/returnc/pub/ [URIs: savagegrowpluszy.today] -0.0 SPF_PASS SPF: sender matches SPF record 0.0 SPF_HELO_NONE SPF: HELO does not publish an SPF Record 2.7 RCVD_IN_PSBL RBL: Received via a relay in PSBL [62.197.136.175 listed in psbl.surriel.com] 1.2 URIBL_ABUSE_SURBL Contains an URL listed in the ABUSE SURBL blocklist [URIs: savagegrowpluszy.today] 0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or identical to background 0.0 HTML_MESSAGE BODY: HTML included in message 0.4 PP_MIME_FAKE_ASCII_TEXT BODY: MIME text/plain claims to be ASCII but isn't 0.1 DKIM_SIGNED Message has a DKIM or DK signature, not necessarily valid -0.1 DKIM_VALID_EF Message has a valid DKIM or DK signature from envelope-from domain -0.1 DKIM_VALID Message has at least one valid DKIM or DK signature -0.1 DKIM_VALID_AU Message has a valid DKIM or DK signature from author's domain 1.9 RAZOR2_CF_RANGE_51_100 Razor2 gives confidence level above 50% [cf: 100] 0.9 RAZOR2_CHECK Listed in Razor2 (http://razor.sf.net/) 0.8 RDNS_NONE Delivered to internal network by a host with no rDNS 0.0 T_REMOTE_IMAGE Message contains an external image --550dd8586b4db0d1699ab199eea250cc_16e30_60e51 Content-Type: text/plain; Content-Transfer-Encoding: 8bit Order Now To Get A Special 5O% OFF http://savagegrowpluszy.today/M4PHCRll5MeIrJJmmPFkKESPfY-0932eLGEz9q4Kyd1up3BmuQ http://savagegrowpluszy.today/tG1Kq7dXa32RnPXibXd2yJdhmoRZu91GFT40f9Duk0TljnqrUw During the Albian to Turonian (93.9 – 89.8 ± 0.3 million years ago), the carbonate platform rose above the sea by about 100 metres (330 ft)–160 metres (520 ft). This uplift episode at Resolution Guyot is part of an episode of more general tectonic changes in the Pacific Ocean, with a general uplift of the ocean floor and tectonic stress changes at the ocean margins. This tectonic event has been explained by a major change in mantle convection in the middle Cretaceous pushing the ocean floor upward and sideward. When Resolution Guyot rose above sea level, karst processes began to impact the platform. The platform became irregular and part of it was eroded away; calcrete crusts, carbonate pinnacles, cavities, caverns containing speleothems and sinkholes formed and exist to this day. At this stage, Resolution Guyot would have resembled a makatea island. This karstic episode did not last for long, perhaps several hundred thousand years, but structures left by the karstic phase such as sinkholes and carbonate pinnacles can still be seen on the surface platform of Resolution Guyot. During periods of emergence, freshwater flowed through and modified the carbonate --550dd8586b4db0d1699ab199eea250cc_16e30_60e51 Content-Type: text/html; Content-Transfer-Encoding: 8bit

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During the Albian to Turonian (93.9 – 89.8 ± 0.3 million years ago), the carbonate platform rose above the sea by about 100 metres (330 ft)–160 metres (520 ft). This uplift episode at Resolution Guyot is part of an episode of more general tectonic changes in the Pacific Ocean, with a general uplift of the ocean floor and tectonic stress changes at the ocean margins. This tectonic event has been explained by a major change in mantle convection in the middle Cretaceous pushing the ocean floor upward and sideward. When Resolution Guyot rose above sea level, karst processes began to impact the platform. The platform became irregular and part of it was eroded away; calcrete crusts, carbonate pinnacles, cavities, caverns containing speleothems and sinkholes formed and exist to this day. At this stage, Resolution Guyot would have resembled a makatea island. This karstic episode did not last for long, perhaps several hundred thousand years, but structures left by the karstic phase such as sinkholes and carbonate pinnacles can still be seen on the surface platform of Resolution Guyot. During periods of emergence, freshwater flowed through and modified the carbonate
 
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