From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #10554 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 10554 Today's Subjects: ----------------- Kid Caught in Blizzard - THIS Kept Him Alive ["Sleeping Bag" Subject: Kid Caught in Blizzard - THIS Kept Him Alive Kid Caught in Blizzard - THIS Kept Him Alive http://themagicenergy.shop/FS1Y5Jycidt1xk5EFCeRCas07KjI8iUZtRDz7cPBIQkToaS9AA http://themagicenergy.shop/8dFA1cKQhGUK6BgzkVWXYTuYjqmkWXMwRhZOy2dmcIKU3GMZ-w 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 to the caldera have been buried by sediments, or soil development has set in. Wind removed the volcanic ash, leaving block and lapilli sized pebbles that cover most of the deposits; in some places dunes have formed from pebbles. Pyroclastic flows also formed, perhaps through instability of the eruption column (unit "CB23"), and spread away from the volcano through surrounding valleys. They reached distances of 35 kilometres (22 mi) from Cerro Blanco and while many of their up to 30-metre (98 ft) thick deposits are heavily eroded well-exposed outcrops occur south of the volcano at Las Papas. They consist of pumice fragments of varying sizes embedded within ash ------------------------------ End of alt.music.moxy-fruvous digest V14 #10554 ***********************************************