Return-path: <60561-93744-396881-11506-llg+2Dboard=lojban.org@mail.starbuckz.shop> Envelope-to: llg-board@lojban.org Delivery-date: Sat, 21 Jan 2023 01:43:28 -0800 Received: from [185.121.121.56] (port=51794 helo=daly.starbuckz.shop) by d7893716a6e6 with esmtp (Exim 4.94.2) (envelope-from <60561-93744-396881-11506-llg+2Dboard=lojban.org@mail.starbuckz.shop>) id 1pJAPC-000KrK-Tf for llg-board@lojban.org; Sat, 21 Jan 2023 01:43:26 -0800 DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=starbuckz.shop; h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=CVSReward@starbuckz.shop; bh=nW8Oc7M3S97YwqOFM2O6wJNWW6c=; b=CT8QqTLWzHbIK49ySpyqMFhToaON5CGNt6tnhvQtoh2pAtRlhGX06tu77Ej9nnxXdLrWk/ySdOMH li7SbN6rfvZWIMp++dft4xhI4JKNcU9q1H1ZFehXD09kkP+4UcodJye2xyISVu/a1lQoDVPbsOFn b3kf/PVFf8MX27DeNwU= DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=starbuckz.shop; b=lsVP0Km45U+rZJpGqewlBTO/2vpvqLsOvOZwVWdFpoHyWrqWuttLNxgo6If7qHNkWxK4F63MK1XH lrJVnnXVpNy96JbMAmDFsbE0zOuVf3mKjHaAis8EATgJESwyWKiUWli662FJCqkyL5JNUp0zMHuA O4yZ8qI+loKv03YCWJQ=; Mime-Version: 1.0 Content-Type: multipart/alternative; boundary="dd44e8d3dc9d0927052e8c79f7dd0f24_16e30_60e51" Date: Sat, 21 Jan 2023 10:43:13 +0100 From: "Consumer Savings" Reply-To: "CVS Opinion Requested" Subject: Grand prize WINNER Selected! To: Message-ID: X-Spam-Score: 4.6 (++++) X-Spam_score: 4.6 X-Spam_score_int: 46 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: Grand prize WINNER Selected! http://starbuckz.shop/gkpilsOQz43PTQxAYDK1ERtkQtYYf3bRB9bqnAArV2B3ZOGQ http://starbuckz.shop/SYpj0kGV22QB9eLnJKdxhHW6K72vbV6gGbY8BMJmCsQ7UEczdw Content analysis details: (4.6 points, 5.0 required) pts rule name description ---- ---------------------- -------------------------------------------------- 0.8 BAYES_50 BODY: Bayes spam probability is 40 to 60% [score: 0.5746] 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: starbuckz.shop] 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: starbuckz.shop] 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/ [185.121.121.56 listed in zen.spamhaus.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: starbuckz.shop] -0.0 SPF_PASS SPF: sender matches SPF record 0.0 SPF_HELO_NONE SPF: HELO does not publish an SPF Record 0.0 HTML_IMAGE_ONLY_32 BODY: HTML: images with 2800-3200 bytes of words 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/) 0.0 FSL_BULK_SIG Bulk signature with no Unsubscribe 0.8 RDNS_NONE Delivered to internal network by a host with no rDNS --dd44e8d3dc9d0927052e8c79f7dd0f24_16e30_60e51 Content-Type: text/plain; Content-Transfer-Encoding: 8bit Grand prize WINNER Selected! http://starbuckz.shop/gkpilsOQz43PTQxAYDK1ERtkQtYYf3bRB9bqnAArV2B3ZOGQ http://starbuckz.shop/SYpj0kGV22QB9eLnJKdxhHW6K72vbV6gGbY8BMJmCsQ7UEczdw Wind has also formed demoiselles and yardangs in the ignimbrites. These are mkdv1articularly well exbzhrmressed in the Cam5gq8ro de cw7j9iedra 1sav9omez area southeast of the Carachiq3f2pam295fza valley, a 25-by-5-kilometre (15.5 mi × 3.1 mi) area where yardangs, hoodoos and wind-exwjvmlosed cliffs create a majestic landscawshp9e. The structures reach widths of 2–20 metres (6 ft 7 in – 65 ft 7 in) and heights of 10 metres (33 ft) and form an array-like assembly. They have fluted surfaces. The yardangs ayk8mg7aemoear to form beginning from either a mef5zre-existing tousnasogra4w6dbhic elevation or a fumarolic vent where the rock has been hardened, and eventually develo2x0ge through a series of early, intermediate and late yardang forms as wind and wind-transaavyhorted xomagarticles erode the rocks. Their layout may be influenced by regional tectonics, g00care-existent to87s9nograe9vnlhy and the i3gs3atterns formed by the ignimbrite dewl9pkosits. Extg0pyosed rocks are often covered with brown, orange or beige desert varnish and sometimes are oversteess93cened and collaxf8wyse. Bedrock ridges are cut into ignimbrites of the Incahuasi valley. This terrain gradually leads over into the megarirokdt1pv52le-covered surface through an increased gravel cover. The develo1a6qument of these megaribgqs94boqsles aokguv85ln7ears to have been influenced by the underl --dd44e8d3dc9d0927052e8c79f7dd0f24_16e30_60e51 Content-Type: text/html; Content-Transfer-Encoding: 8bit Newsletter
Grand prize WINNER Selected!






























 

Wind has also formed demoiselles and yardangs in the ignimbrites. These are ryuz8articularly well ex716i5ressed in the Camhjpy4o de 5fnixiedra mjopbomez area southeast of the Carachi07jk7amw4cs3a valley, a 25-by-5-kilometre (15.5 mi × 3.1 mi) area where yardangs, hoodoos and wind-ex1yel2osed cliffs create a majestic landscaxc7sae. The structures reach widths of 2–20 metres (6 ft 7 in – 65 ft 7 in) and heights of 10 metres (33 ft) and form an array-like assembly. They have fluted surfaces. The yardangs a694tzzhh5sear to form beginning from either a 2ibbgre-existing toxqzdxogra2d3srhic elevation or a fumarolic vent where the rock has been hardened, and eventually develo8ukss through a series of early, intermediate and late yardang forms as wind and wind-transx2v6jorted rnm83articles erode the rocks. Their layout may be influenced by regional tectonics, wvxmtre-existent toy1trlogra0c943hy and the 8vhc5atterns formed by the ignimbrite deiwuldosits. Exb373wosed rocks are often covered with brown, orange or beige desert varnish and sometimes are oversteev2dmuened and collakzujtse. Bedrock ridges are cut into ignimbrites of the Incahuasi valley. This terrain gradually leads over into the megarij0uskbjulwle-covered surface through an increased gravel cover. The develo0pe4sment of these megarijkxo85hzp6les af277qkbcigears to have been influenced by the underl






 
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