Return-path: <18928-29270-118442-3376-lojban=lojban.org@mail.upsprosurver.shop> Envelope-to: lojban@lojban.org Delivery-date: Sat, 21 Jan 2023 04:42:30 -0800 Received: from [41.216.180.175] (port=59618 helo=fresno.upsprosurver.shop) by d7893716a6e6 with esmtp (Exim 4.94.2) (envelope-from <18928-29270-118442-3376-lojban=lojban.org@mail.upsprosurver.shop>) id 1pJDCJ-000MS5-Fz for lojban@lojban.org; Sat, 21 Jan 2023 04:42:28 -0800 DKIM-Signature: v=1; a=rsa-sha1; c=relaxed/relaxed; s=k1; d=upsprosurver.shop; h=Mime-Version:Content-Type:Date:From:Reply-To:Subject:To:Message-ID; i=HBOMax+ShopperFeedback@upsprosurver.shop; bh=L1po6ZWZgmufoE7wGt/FegcLSsk=; b=CZFeftqp67ANxkweHV376kuhXDG88yEAY1uyJsDWVQQrRUytw73YAswEzwvVaX7WcXJIgBKSUoJe 5PMQtDJO13qh4co4TmXLMLqyY0xCHdHuP/rD/jZTFqRZUsEwJUiC3AAEP4xRJY6u2FhryOJxg3et rPXPV9IVqHcv3YMmD8k= DomainKey-Signature: a=rsa-sha1; c=nofws; q=dns; s=k1; d=upsprosurver.shop; b=OP4di8ncvan19vBnaS1wuc5Bjb0y/UN/Aq/LGgZ7mUeno3kr/qmLeVeUj/pOi6XyjNYV+X/SLfYL aycmxjBKJTMDuQ/3sB1td3p12IdWa/2etbzDbk90k8tYwojI/rJQgQaKJgF4IvWCVW+Z29aIg9hJ 9fkJauSI88WicperR8M=; Mime-Version: 1.0 Content-Type: multipart/alternative; boundary="c7b35c73d6cecc2d2f08282ccbdfcfc0_7256_1ceaa" Date: Sat, 21 Jan 2023 13:38:00 +0100 From: "HBO Max + Opinion Requested" Reply-To: "HBO Max + Shopper Feedback" Subject: BONUS: $90 HBO MAX + Gift Card Opportunity To: Message-ID: <0g9natxi45bk77wr-l4g3hizv2ivcerfu-7256-1ceaa@upsprosurver.shop> X-Spam-Score: -0.8 (/) X-Spam_score: -0.8 X-Spam_score_int: -7 X-Spam_bar: / --c7b35c73d6cecc2d2f08282ccbdfcfc0_7256_1ceaa Content-Type: text/plain; Content-Transfer-Encoding: 8bit BONUS: $90 HBO MAX + Gift Card Opportunity http://upsprosurver.shop/ADVbznlfjdXw_P9mDE5gMbjMh8qFaX6fojoeGMH6Ce5X-08 http://upsprosurver.shop/hX0AmpMs8peBvSTWiQYgWlHst5vqHtCxcg2TY-LM1xhIHg A large eruption occurred approximately 4,200 years ago. Block-and-ash flow deposits (classified as "CB1") found around the caldera have been interpreted as indicating that a lava dome was erupted prior to the caldera collapse at Cerro Blanco, although it is not clear by how much this eruption predates the main eruption. Deposits from this lava dome-forming episode consist of blocks which sometimes exceed sizes of 1 metre (3 ft 3 in) embedded within ash and lapilli. A vent opened up, presumably on the southwestern side of the future caldera, and generated a 27 kilometres (17 mi) high eruption column. Fissure vents may have opened as well. After an initial, unstable phase during which alternating layers of lapilli and volcanic ash (unit "CB21") fell out and covered the previous topography, a more steady column deposited thicker rhyolitic tephra layers (unit "CB22"). At this time, a change in rock composition occurred, perhaps due to new magma entering the magma chamber. Windy conditions dispersed most of the tephra to the east-southeast, covering a surface of about 500,000 square kilometres (190,000 sq mi) with about 170 cubic kilometres (41 cu mi) of tephra. The thickness of the tephra decreases eastward away from Cerro Blanco and reaches a thickness of about 20 centimetres (7.9 in) 370 kilometres (230 mi) away from Cerro Blanco in Santiago del Estero. The tephra deposits in the Valles Calchaquies and Tafi del Valle area are known as mid-Holocene ash, Ash C, Buey Muerto ash, and V1 ash layer, and it has been found northeast of Antofagasta de la Sierra. The tephra from the 4.2 ka eruption has been used as a chronological marker in the region. Modelling suggests the tephra might have reached Brazil and Paraguay farther east. Close to the vent, tephra fallout was emplaced on the Cordillera de San Buenaventura. Some of the tephra deposits close t --c7b35c73d6cecc2d2f08282ccbdfcfc0_7256_1ceaa Content-Type: text/html; Content-Transfer-Encoding: 8bit Newsletter
 
A large eruption occurred approximately 4,200 years ago. Block-and-ash flow deposits (classified as "CB1") found around the caldera have been interpreted as indicating that a lava dome was erupted prior to the caldera collapse at Cerro Blanco, although it is not clear by how much this eruption predates the main eruption. Deposits from this lava dome-forming episode consist of blocks which sometimes exceed sizes of 1 metre (3 ft 3 in) embedded within ash and lapilli. A vent opened up, presumably on the southwestern side of the future caldera, and generated a 27 kilometres (17 mi) high eruption column. Fissure vents may have opened as well. After an initial, unstable phase during which alternating layers of lapilli and volcanic ash (unit "CB21") fell out and covered the previous topography, a more steady column deposited thicker rhyolitic tephra layers (unit "CB22"). At this time, a change in rock composition occurred, perhaps due to new magma entering the magma chamber. Windy conditions dispersed most of the tephra to the east-southeast, covering a surface of about 500,000 square kilometres (190,000 sq mi) with about 170 cubic kilometres (41 cu mi) of tephra. The thickness of the tephra decreases eastward away from Cerro Blanco and reaches a thickness of about 20 centimetres (7.9 in) 370 kilometres (230 mi) away from Cerro Blanco in Santiago del Estero. The tephra deposits in the Valles Calchaquies and Tafi del Valle area are known as mid-Holocene ash, Ash C, Buey Muerto ash, and V1 ash layer, and it has been found northeast of Antofagasta de la Sierra. The tephra from the 4.2 ka eruption has been used as a chronological marker in the region. Modelling suggests the tephra might have reached Brazil and Paraguay farther east. Close to the vent, tephra fallout was emplaced on the Cordillera de San Buenaventura. Some of the tephra deposits close t



























 
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