Return-path: <52759-93744-396881-13312-llg+2Dboard=lojban.org@mail.counselo.za.com> Envelope-to: llg-board@lojban.org Delivery-date: Wed, 22 Jun 2022 07:28:57 -0700 Received: from [109.236.49.205] (port=58395 helo=reno.counselo.za.com) by d05c5d92ccf2 with esmtp (Exim 4.94.2) (envelope-from <52759-93744-396881-13312-llg+2Dboard=lojban.org@mail.counselo.za.com>) id 1o41Lh-003BQd-Tr for llg-board@lojban.org; Wed, 22 Jun 2022 07:28:55 -0700 DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=counselo.za.com; h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=DangerousHormones@counselo.za.com; bh=Ttenv0epm9Z61P05nHNkR2+5keo=; b=wiod+vEm4wiqUdsqqVljCdTY4w3XTYocPE64z++EyAsR63usX5JHp95V3X6On6ytoJ240mtAvBgu uWI3bgN6/P66deQNK0SrBAT46AQmvq6owldrvqFkEuc1/uxytMNohJqMCfNHuF5TzaC5sfan1gSe ndos56KSp70QFRSULXE= DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=counselo.za.com; b=ZZ7ihorel2m3imRiu70mEPowAYYvip58zjhJD2bjH/hM1GWVhK9yaLyH1sFEQ6hCA90Qpr1JvyXG vUUcukh2yfBYipD4OfFQDZUxBXGGhlJipgak3VDWtY2vbMW/gA1LcI0vU8nLof/ZyF/PsqnT3QTR 7kQ+2ujVdj9DdjN9kM8=; Mime-Version: 1.0 Content-Type: multipart/alternative; boundary="95bb63a00a5304111b103dca0fab046b_16e30_60e51" Date: Wed, 22 Jun 2022 09:43:31 -0400 From: "Dangerous Hormones" Reply-To: "3 DEADLY fruits" <3DEADLYfruits@counselo.za.com> Subject: Are you eating these 3 DANGEROUS fruits? To: Message-ID: <9al2uvcts02cxden-i2s9u92cs9vukbey-16e30-60e51@counselo.za.com> X-Spam-Score: 1.1 (+) X-Spam_score: 1.1 X-Spam_score_int: 11 X-Spam_bar: + X-Spam-Report: Spam detection software, running on the system "bcda1c85505f", 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: Are you eating these 3 DANGEROUS fruits? http://counselo.za.com/HKtxt0FmMd59SZSddZfgkgDog7lDzX_7qYhcGhy1Qdvrryjg http://counselo.za.com/874-qs29vsr_BzLjOY1nDRelSgWfO-_2PYPgBMy8ZWKno9730A Content analysis details: (1.1 points, 5.0 required) pts rule name description ---- ---------------------- -------------------------------------------------- 1.5 BAYES_60 BODY: Bayes spam probability is 60 to 80% [score: 0.6779] 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: counselo.za.com] -5.0 RCVD_IN_DNSWL_HI RBL: Sender listed at https://www.dnswl.org/, high trust [109.236.49.205 listed in list.dnswl.org] 1.2 URIBL_ABUSE_SURBL Contains an URL listed in the ABUSE SURBL blocklist [URIs: counselo.za.com] 2.7 RCVD_IN_PSBL RBL: Received via a relay in PSBL [109.236.49.205 listed in psbl.surriel.com] 0.0 SPF_HELO_NONE SPF: HELO does not publish an SPF Record 0.0 T_SPF_PERMERROR SPF: test of record failed (permerror) 0.0 HTML_MESSAGE BODY: HTML included in message 0.0 HTML_FONT_LOW_CONTRAST BODY: HTML font color similar or identical to background -0.1 DKIM_VALID_AU Message has a valid DKIM or DK signature from author's domain -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_SIGNED Message has a DKIM or DK signature, not necessarily valid 0.8 RDNS_NONE Delivered to internal network by a host with no rDNS --95bb63a00a5304111b103dca0fab046b_16e30_60e51 Content-Type: text/plain; Content-Transfer-Encoding: 8bit Are you eating these 3 DANGEROUS fruits? http://counselo.za.com/HKtxt0FmMd59SZSddZfgkgDog7lDzX_7qYhcGhy1Qdvrryjg http://counselo.za.com/874-qs29vsr_BzLjOY1nDRelSgWfO-_2PYPgBMy8ZWKno9730A re strongest near the surface, though the geochemical influences on soil properties increase with depth. Mature soil profiles typically include three basic master horizons: A, B, and C. The solum normally includes the A and B horizons. The living component of the soil is largely confined to the solum, and is generally more prominent in the A horizon. It has been suggested that the pedon, a column of soil extending vertically from the surface to the underlying parent material and large enough to show the characteristics of all its horizons, could be subdivided in the humipedon (the living part, where most soil organisms are dwelling, corresponding to the humus form), the copedon (in intermediary position, where most weathering of minerals takes place) and the lithopedon (in contact with the subsoil). The soil texture is determined by the relative proportions of the individual particles of sand, silt, and clay that make up the soil. The interaction of the individual mineral particles with organic matter, water, gases via biotic and abiotic processes causes those particles to flocculate (stick together) to form aggregates or peds. Where these aggregates can be identified, a soil can be said to be developed, and can be described further in terms of color, porosity, consistency, reaction (acidity), etc. Water is a critical agent in soil de --95bb63a00a5304111b103dca0fab046b_16e30_60e51 Content-Type: text/html; Content-Transfer-Encoding: 8bit Newsletter
Hey,

Are you eating these 3 DANGEROUS fruits?



These 3 fruits increase the levels of "dangerous hormones" in your body…

You know.. The kind of hormones that destroy a healthy heart and increases your risk of heart attack by 77%…

The bad news is…

These 3 fruits are among America's favorites and are commonly found in fridges.

Is it in your fridge too?

Sincerely,
Pansy










 








re strongest near the surface, though the geochemical influences on soil properties increase with depth. Mature soil profiles typically include three basic master horizons: A, B, and C. The solum normally includes the A and B horizons. The living component of the soil is largely confined to the solum, and is generally more prominent in the A horizon. It has been suggested that the pedon, a column of soil extending vertically from the surface to the underlying parent material and large enough to show the characteristics of all its horizons, could be subdivided in the humipedon (the living part, where most soil organisms are dwelling, corresponding to the humus form), the copedon (in intermediary position, where most weathering of minerals takes place) and the lithopedon (in contact with the subsoil). The soil texture is determined by the relative proportions of the individual particles of sand, silt, and clay that make up the soil. The interaction of the individual mineral particles with organic matter, water, gases via biotic and abiotic processes causes those particles to flocculate (stick together) to form aggregates or peds. Where these aggregates can be identified, a soil can be said to be developed, and can be described further in terms of color, porosity, consistency, reaction (acidity), etc. Water is a critical agent in soil de





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