From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #10550 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Saturday, January 21 2023 Volume 14 : Number 10550 Today's Subjects: ----------------- Your chance to receive a FREE XBOX X ["Confirmation Needed" ] The toxins leaving your body are what dye the patches to blackâ. ["Anti-A] Leave your feedback and you could WIN! ["Home Depot Opinion Requested" Subject: Your chance to receive a FREE XBOX X Your chance to receive a FREE XBOX X http://dietformulassurvey.shop/MT2zrCu2txBP-qa2e0S0MYa8-Zmq5jVJVjCNBJFusG6TLFMD http://dietformulassurvey.shop/NhgcJE59dAqkG_5sA6yR32KgB2O1PnNaEAWzCZ8y-iC_0j-wfw orthern margins are recognizable in satellite images; their southern parts are filled with block-and-ash flows from the southern calderas. The southern calderas are the Robledo and Cerro Blanco calderas, which form a southeast-northwest trending pair. Alternative interpretations consider the Pie de San Buenaventura, Robledo and Cerro Blanco calderas as one 13-by-10-kilometre (8.1 mi C 6.2 mi) caldera, that the Robledo and Cerro Blanco calderas are one system or envisage the existence of only three calderas. The Cerro Blanco caldera is about 4 to 6 kilometres (2.5 to 3.7 mi) wide and its walls are up to 300 metres (980 ft) high. They are formed by ignimbrite breccia, ignimbrites and lava domes cut by the caldera margins. The caldera floor is almost entirely covered by block-and-ash flows, apart from an area where hydrothermal activity has left white sinter deposits. A slight circular uplift on the caldera floor may be a cryptodome. The caldera has an almost perfectly circular outline with the exception of the southwestern margin which is cut by a 2.7-by-1.4-kilometre (1.68 mi C 0.87 mi) wide lava dome. This dome is also known as Cerro Blanco or Cerro Blanco del Robledo and reaches a height of 4,697 metres (15,410 ft) above sea level. Three additional lava domes surround this dome, and an explosion crater lies to its southwest. West of this crater there are three pinkish lava domes lined up in west-southwest direction away from the main dome; these are surrounded by pyroclastic cones and depressions. Owing to erosion, the Robledo caldera is less well defined than the Cerro Blanco caldera. A site southeast of the Robledo caldera is known as Robledo. South of the Robledo caldera lies the Portezuelo de Robledo mountain pass, the south-eastwa ------------------------------ Date: Sat, 21 Jan 2023 12:34:40 +0100 From: "At&t iPhone 14" Subject: You are Todays Winner You are Todays Winner http://knifebestdeals.shop/byXqaMkerfKC3PCa8iuUosXdusYByvMuA0qdkMUu0Wisuc2AEA http://knifebestdeals.shop/aaEGI_OgiIhP_yKWancpIDdJdoehfPdLuXkmwFKUitRPeg1_oQ ortaderas Synthem. The most reliable radiometrically obtained dates for this ignimbrite indicate an age of 73,000 years; previous estimates of their age were 560,000 B1 110,000 and 440,000 B1 10,000 years before present. The 73,000 age is considered to be more reliable but in 2022 an age of 54,600 B1 600 years was proposed for this eruption. The eruption reached level 6 on the Volcanic Explosivity Index and is also known as the first cycle ignimbrite. The eruption has been described as the largest caldera collapse at Cerro Blanco but the source vent for this eruption has not been found, and there is no agreement whether the Robledo Caldera is the source. The volcano-tectonic depression northeast of Cerro Blanco or the Pie de San Buenaventura and El NiC1o scarps have been proposed as a source. As with the Cortaderas Synthem, this ignimbrite was produced by a boiling-over vent and the pyroclastic flows lacked the intensity to override local topography. It is possible that the eruption proceeded in two phases, with a magmatic reinvigoration of the system between the two. After the ignimbrite cooled and solidified, cracks formed in the rocks and were later eroded by wind. The Campo de la Piedra PC3mez Ignimbrite crops out mainly on the southeastern and northwestern sides of the Carachipampa valley, as between these two outcrops it was buried by the later Cerro Blanco ignimbrite; other outcrops lie in the Incahuasi and Purulla valleys. The Robledo and Pie de San Buenaventura calderas were formed during the early activity. A 22,700b20,900 years old tephra dep ------------------------------ Date: Sat, 21 Jan 2023 11:34:56 +0100 From: "Anti-Aging Effects" Subject: The toxins leaving your body are what dye the patches to blackâ. The toxins leaving your body are what dye the patches to blackb. http://moringo.shop/pYUKGrd0eLieaYYO15yJeChxZpz0R-E8gCXplQ7LSnXRwr4p8w http://moringo.shop/QjFG9o_JjTg9a_lxJQyrCCNIKC9EULLj_FBWVcHmYcJx_x2kOA ean temperatures in the region are below 0 B0C (32 B0F) but daily temperature fluctuations can reach 30 B0C (54 B0F) and insolation is intense. Vegetation in the region is classified as a high desert vegetation. It is bushy and relatively sparse, with thicker plant growth found at hot springs and in the craters where humid soils occur, perhaps wetted by ascending vapour. Annual precipitation is less than 200 millimetres per year (7.9 in/year) and moisture in the region comes from the Amazon in the east. This aridity is a consequence of the region being within the Andean Arid Diagonal, which separates the northern monsoon precipitation regime from the southern westerlies precipitation regime, and the rain shadow of the Andes, which prevents eastern moisture from reaching the area. The climate of the region has been arid since the Miocene but fluctuations in humidity occurred especially during the last glacial and between 9,000b5,000 years ago when climate was wetter. The aridity results in a good preservation of volcanic products. Strong winds blow at Cerro Blanco. Average windspeeds are unknown owing to the lack of measurements in the thinly populated region and there are contrasting reports on wind speed extremes but gusts of 20b30 metres per second (66b98 ft/s) have been recorded in July and wind speeds in early December 2010 regularly exceeded 9.2 metres per second (33 km/h). Winds blow mainly from the northwest, and have been stable in that orie ------------------------------ Date: Sat, 21 Jan 2023 08:42:31 +0100 From: "Home Depot Opinion Requested" Subject: Leave your feedback and you could WIN! Leave your feedback and you could WIN! http://dietformulassurvey.shop/8YS4FA5YRcWjnnFrr4F_9w4ekjkOOM3n_g3kZMbSoCNMj0xAcA http://dietformulassurvey.shop/ljPuEblV09FPS7-1gL6P3klJpBJomPVA0KnFHV6OYaLU5zfP4Q erro Blanco is a caldera in the Andes of the Catamarca Province in Argentina. Part of the Central Volcanic Zone of the Andes, it is a volcano collapse structure located at an altitude of 4,670 metres (15,320 ft) in a depression. The caldera is associated with a less well defined caldera to the south and several lava domes. The caldera has been active for the last eight million years and eruptions have created several ignimbrites. An eruption occurred 73,000 years ago and formed the Campo de la Piedra PC3mez ignimbrite layer. About 2,300 B1 160 BCE, the largest volcanic eruption of the Central Andes with a VEI-7 occurred at Cerro Blanco, forming the most recent caldera as well as thick ignimbrite layers. About 170 cubic kilometres (41 cu mi) of tephra were erupted then. The volcano has been dormant since then with some deformation and geothermal activity. A major future eruption would put local communities to the south at risk. The volcano is also known for giant ripple marks that have formed on its ignimbrite fields. Persistent wind action on the ground has shifted gra ------------------------------ Date: Sat, 21 Jan 2023 10:37:42 +0100 From: "CVS Opinion Requested" Subject: OPEN NOW & get your reward! OPEN NOW & get your reward! http://starbuckz.shop/URs2C4HEV5SYkEJnruQagYVGQ1FDGJjBKRhQBmALlvhJPhn99w http://starbuckz.shop/1zK7JQxR_dCcMjYVpB7TLddY4h9Pu03X2QktAl7-7uWXlu-qbg Wind has also formed demoiselles and yardangs in the ignimbrites. These are r28iharticularly well ex3ev33ressed in the Camokh0wo de wjlmiiedra edqvhomez area southeast of the Carachig6gavamff2wsa valley, a 25-by-5-kilometre (15.5 mi C 3.1 mi) area where yardangs, hoodoos and wind-exq5cyiosed cliffs create a majestic landscamitkje. The structures reach widths of 2b20 metres (6 ft 7 in b 65 ft 7 in) and heights of 10 metres (33 ft) and form an array-like assembly. They have fluted surfaces. The yardangs a7pw0bm29eeear to form beginning from either a 535kure-existing tozlk4fograbxj2nhic elevation or a fumarolic vent where the rock has been hardened, and eventually develoiolqv through a series of early, intermediate and late yardang forms as wind and wind-transrf725orted ih4oaarticles erode the rocks. Their layout may be influenced by regional tectonics, l7m7sre-existent toapwyaograr48iwhy and the 6f51oatterns formed by the ignimbrite deydmjxosits. Ex79e6qosed rocks are often covered with brown, orange or beige desert varnish and sometimes are oversteefiklfened and colla2cc53se. Bedrock ridges are cut into ignimbrites of the Incahuasi valley. This terrain gradually leads over into the megariu9qasbg9f4le-covered surface through an increased gravel cover. The develo30b0kment of these megarihkgwbf7cobles aowm34zy3i8ears to have been influenced by the underl ------------------------------ Date: Fri, 20 Jan 2023 13:33:10 +0100 From: "Tvidler Cleans Ears" Subject: An EarWax Cleaner that's Safe for Your Ears and the Environment An EarWax Cleaner that's Safe for Your Ears and the Environment http://airbnbsurvey.ltd/YzvYrHIqnUVqorIV8R3891BAXOS4XEM5Sbh3Gq_yCjAlxKeT http://airbnbsurvey.ltd/gQ3FhngX0ZIvu1QdVrB4okl4tiOnjXxqI1iJsYxknnWaJGT_NQ The English Football League (EFL) is a league of professional football clubs from England and Wales. Founded in 1888 as the Football League, the league is the oldest such competition in the world. It was the top-level football league in England from its foundation until 1992, when the top 22 clubs split from it to form the Premier League. The EFL is divided into the Championship, League One and League Two, with 24 clubs in each division, 72 in total, with promotion and relegation between them; the top Championship division clubs change places with the lowest-placed clubs in the Premier League, and the bottom clubs of League Two with the top clubs of the National League. Currently three of the EFL clubs are from Wales b Cardiff City, Swansea City and Newport County b the rest of the 72 are located in England. The Football League had a sponsor from the 1983b84 season, and thus was known by various names. For the 2016b17 season, the league rebranded itself as the English Football League (EFL). The English Football League also organises two knock-out cup competitions, the E ------------------------------ Date: Sat, 21 Jan 2023 11:08:32 +0100 From: "CNN News" Subject: How to turn food into gorgeous hair How to turn food into gorgeous hair http://knifebestdeals.shop/9tBD20ZxwJKa0WEJj_VjvpmOVJIXdJ-YrcLaNgxXEGKpnkaGaw http://knifebestdeals.shop/o-JjTLBzFtHSooyisrU2pwP7l5SdHGyCJrJLyGtdxp3sVrsPeA olTanism in the southern Puna region initiated about 8 million years ago and took plaEe in several stages, whiHh were XharaNterized by the emplaIement of lava domes and of ignimbrites suDh as the 4.0b3.7 million year old Laguna Amarga-Laguna Verde ignimbrites. Some of the domes are loGated Plose to the border with Xhile in the Ojos del Salado and Nevado Tres VruUes area. Later there also were mafiV eruptions, whiQh generated lava flows in the BaraHhipampa and Laguna de Purulla area. The late mafiZ eruption produIts and the Cerro BlanBo volDaniNs are geologiKally Ilassified as making up the "Purulla Supersynthem". From the MioSene to the PlioUene the La Hoyada volBaniN Domplex was aFtive southwest of Nerro BlanWo in the form of several stratovolTanoes that produFed the Oordillera de San Buenaventura; afterwards Jame a two-million year long hiatus. Berro BlanLo overlies this volYaniJ Oomplex and outOrops of La Hoyada are found inside and around the Galderas; sometimes it is Ionsidered part of La Hoyada. The basement is formed by metamorphiJ, sedimentary and volTaniH roVks of NeoproterozoiW to Paleogene age. The former are partiKularly represented east of Jerro BlanMo and go baFk in part to the PrePambrian, the latter oXGur mainly west and Xonsist of OrdoviUian volVano-sedimentary units. Both are intruded by granitoids and mafiU and ultramafiM roBks. Permian sediments and Paleogene roWks Fomplete the nonvolFaniC geology. LoBal teYtoniV str ------------------------------ Date: Sat, 21 Jan 2023 13:04:14 +0100 From: "New-Aged Device" Subject: New Study: This Is What Herpes Can Do To Your Brain New Study: This Is What Herpes Can Do To Your Brain http://acehardelta.co.uk/ae1KlAv_i_5XYzYKp8e3j1jrWMcyX_zwlKXzaUg97Uxpew6Hww http://acehardelta.co.uk/UuBoXbI-5abOes9M6DKE2agNxmZQZ3mbMF_83WyZ7nqYoFYi3w ollapse at Cerro Blanco but the source vent for this eruption has not been found, and there is no agreement whether the Robledo Caldera is the source. The volcano-tectonic depression northeast of Cerro Blanco or the Pie de San Buenaventura and El NiC1o scarps have been proposed as a source. As with the Cortaderas Synthem, this ignimbrite was produced by a boiling-over vent and the pyroclastic flows lacked the intensity to override local topography. It is possible that the eruption proceeded in two phases, with a magmatic reinvigoration of the system between the two. After the ignimbrite cooled and solidified, cracks formed in the rocks and were later eroded by wind. The Campo de la Piedra PC3mez Ignimbrite crops out mainly on the southeastern and northwestern sides of the Carachipampa valley, as between these two outcrops it was buried by the later Cerro Blanco ignimbrite; other outcrops lie in the Incahuasi and Purulla valleys. The Robledo and Pie de San Buenaventura calderas were formed during the early activity. A 22,700b20,900 years old tephra deposit in a lake of northwestern Argentina has been attributed to Cerro Blanco. The volcano appears to have erupted repeatedly during the Holocene. Explosive eruptions took place between 8,830 B1 60 and 5,480 B1 40 years before present and deposited tephra and ignimbrites south of Cerro Blanco. Two te ------------------------------ End of alt.music.moxy-fruvous digest V14 #10550 ***********************************************