[44774] in linux-announce channel archive
The IRS Has Forgiven Millions Through Its Tax Debt Assistance Programs
daemon@ATHENA.MIT.EDU (RS Assistance Programs Federal Tax)
Tue Feb 6 10:14:53 2024
Date: Tue, 6 Feb 2024 16:14:49 +0100
From: "RS Assistance Programs Federal Tax Debt Help" <RSAssistanceProgramsFederalTaxDebtHelp@brainsaviorx.today>
Reply-To: "FTDH" <FederalTaxDebtHelp@brainsaviorx.today>
To: <linuxch-announce.discuss@charon.mit.edu>
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The IRS Has Forgiven Millions Through Its Tax Debt Assistance Programs
http://brainsaviorx.today/WkP0bJe6LcFvg3KViOpwjm8KQgQicfqGPNxY1ZyiqRFb90R5KA
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features 18 central volcanoes and accompanying parasitic vents, which form islands off the coast or nunataks in the ice. Many of these volcanoes form distinct volcanic chains, such as the Executive Committee Range where volcanic activity has shifted westward at a rate of about 1 centimetre per year (0.4 in/year). Such a movement is also apparent in the Flood Range, where activity migrated from Mount Moulton to Mount Berlin. This movement appears to reflect the propagation of crustal fractures, as plate motion is extremely slow in the region. Volcanic activity appears to take place in three phases, an early mafic phase, often followed by a second felsic phase. End-stage volcanism occurs in the form of small cone-forming eruptions. Ignimbrites are rare in Marie Byrd Land; the outcrop on the southeastern flank of Mount Berlin is an uncommon exception.
Activity in the Marie Byrd Land Volcanic Province began during the middle Miocene and continued into the later Quaternary; argon-argon dating yielded ages as young as 8,200 years. Four volcanoes in the Marie Byrd Land Volcanic Province – Mount Berlin, Mount Siple, Mount Takahe and Mount Waesche – were classified as "possibly or potentially active" in the 1990 Antarctic Research Series by LeMasurier et al., and active subglacial volcanoes have been identified on the basis of aerophysical surveys.
The volcanic province is related to the West Antarctic Rift which is interpreted as a rift or as a plate boundary. The West Antarctic Rift has been volcanically and tectonically active over the past 30–25 million years. The basement crops out near the coast and consists of Paleozoic rocks with intruded Cretaceous and Devonian granites which w
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<a href="http://brainsaviorx.today/WkP0bJe6LcFvg3KViOpwjm8KQgQicfqGPNxY1ZyiqRFb90R5KA"><b style="font-size:23;color:#f17859;">The IRS Has Forgiven Millions Through Its Tax Debt Assistance Programs</b></a><br />
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<p style="color:#FFFFFF;font-size:4px;">features 18 central volcanoes and accompanying parasitic vents, which form islands off the coast or nunataks in the ice. Many of these volcanoes form distinct volcanic chains, such as the Executive Committee Range where volcanic activity has shifted westward at a rate of about 1 centimetre per year (0.4 in/year). Such a movement is also apparent in the Flood Range, where activity migrated from Mount Moulton to Mount Berlin. This movement appears to reflect the propagation of crustal fractures, as plate motion is extremely slow in the region. Volcanic activity appears to take place in three phases, an early mafic phase, often followed by a second felsic phase. End-stage volcanism occurs in the form of small cone-forming eruptions. Ignimbrites are rare in Marie Byrd Land; the outcrop on the southeastern flank of Mount Berlin is an uncommon exception. Activity in the Marie Byrd Land Volcanic Province began during the middle Miocene and continued into the later Quaternary; argon-argon dating yielded ages as young as 8,200 years. Four volcanoes in the Marie Byrd Land Volcanic Province – Mount Berlin, Mount Siple, Mount Takahe and Mount Waesche – were classified as "possibly or potentially active" in the 1990 Antarctic Research Series by LeMasurier et al., and active subglacial volcanoes have been identified on the basis of aerophysical surveys. The volcanic province is related to the West Antarctic Rift which is interpreted as a rift or as a plate boundary. The West Antarctic Rift has been volcanically and tectonically active over the past 30–25 million years. The basement crops out near the coast and consists of Paleozoic rocks with intruded Cretaceous and Devonian granites which w</p>
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