From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #13190 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 Tuesday, February 6 2024 Volume 14 : Number 13190 Today's Subjects: ----------------- You have been randomly selected! ["Good News" Subject: You have been randomly selected! You have been randomly selected! http://heartburnnomore.life/tiNIcYOi7Je6haIErHhgCUAJT_iRmskxO_cEqow2TLS95_VxVg http://heartburnnomore.life/ovCqTwPSNEYfK2zZvgTJOTQgTxEwwK1PjgjkRtC112QpQg6N0w 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 b Mount Berlin, Mount Siple, Mount Takahe and Mount Waesche b 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 30b25 million years. The basement crops out near the coast and consists of Paleozoic rocks with intruded Cretaceous and Devonian granites which w ------------------------------ Date: Tue, 6 Feb 2024 14:51:08 +0200 From: reham nomeer Subject: =?UTF-8?B?2KPZgtmI2Ykg2LTZh9in2K/YqSDZgdmKINin2K/Yp9ix2Kkg2KfZh Niq2LrZitmK2LEg?= =?UTF-8?B?2YjZhdinINiy2KfZhCDYudiv2K8g2K3Yp9mF2YTZiiDYp9mE2LTZh9in2K/Y qSDZgtmE2YrZhCDYudmE?= =?UTF-8?B?2Ykg2YXYs9iq2YjZiSDYp9mE2LnYp9mE2YUg2YXZhdinINmK2LLZitivINmF 2YYg2KfZhNmB2LHYtSA=?= =?UTF-8?B?2KfZhNmF2KrYp9it2Kkg2YTZhdmGINmK2K3ZhdmEINmH2LDYpyDYp9mE2YXY pNmH2YQg2YHZiiDYp9mE?= =?UTF-8?B?2YXZhtin2LXYqCDYp9mE2YLZitin2K/ZitipINin2YTYtNmH2KfYr9ipINin 2YTYp9it2KrYsdin2YE=?= =?UTF-8?B?2YrYqSA6LSDZhdit2KrYsdmBINin2K/Yp9ix2Kkg2KfZhNiq2LrZitmK2LEg Q0NNUCDYrtmE2KfZhCA=?= =?UTF-8?B?2KfZhNmB2KrYsdipINmF2YYgMTgg4oCTIDIwINmB2KjZgNmA2YDZgNmA2YDZ gNmA2YDZgNmA2LHYp9mK?= =?UTF-8?B?2LEgMjAyNCDZhdmC2K/ZhdipINmF2YYg2KfZhNiv2KfYsSDYp9mE2LnYsdio 2YrYqSDZhNmE2KrZhtmF?= =?UTF-8?B?2YrYqSDYp9mE2KfYr9in2LHZitipIC0gQUhBRCDYp9mE2YLYp9mH2LHYqSDi gJMg2KzZhdmH2YjYsdmK?= =?UTF-8?B?2Kkg2YXYtdixINin2YTYudix2KjZitipINmF2Lkg2KfZhdmD2KfZhtmK2Kkg 2KfZhNmF2LTYp9ix2YM=?= =?UTF-8?B?2Kkg2KfZiNmGINmE2KfZitmGINi52KjYsSDYstmI2YUg2KfZhNi02YfYp9iv 2Kkg2YXYudiq2YXYr9ip?= =?UTF-8?B?INiv2YjZhNmK2KfZiyDZiCDYrdmD2YjZhdmK2KfZiyDZiCDZhdi52KrYsdmB INio2YfYpyDZgdmKINis?= =?UTF-8?B?2YXZiti5INiv2YjZhCDYp9mE2LnYp9mE2YUg4oCiINiq2LXYr9mK2YIg2YjY stin2LHYqSDYp9mE2K4=?= =?UTF-8?B?2KfYsdis2YrYqSDYp9mE2YXYtdix2YrYqSDZiCDZhdmD2KrYqCDYp9mE2KrY tdiv2YrZgtin2Kog2Kc=?= =?UTF-8?B?2YTZgtmG2LXZhNmKINmF2K3Yp9mI2LEg2KfZhNio2LHZhtin2YXYrDog2KrY udix2YrZgSDYudin2YUg?= =?UTF-8?B?2KjYpdiv2KfYsdipINin2YTYqti62YrZitixINmI2KPZh9mF2YrYqtmHINmB 2Yog2KrYrdmC2YrZgiA=?= =?UTF-8?B?2KfZhNmF2YbYp9mB2LkuINiq2YjYttmK2K0g2KfZhNmF2YHYp9mH2YrZhSDY p9mE2K7vv70=?= X#YYY X4YX'X/X) YY X'X/X'X1X) X'YX*X:Y Y X1 YYX' X2X'Y X9X/X/ X-X'YYY X'YX4YX'X/X) YYY Y X9YY YX3X*YY X'YX9X'YY YYX' Y X2Y X/ YY X'YYX1X5 X'YYX*X'X-X) YYY Y X-YY YX0X' X'YYX$YY YY X'YYYX'X5X( X'YYY X'X/Y X) *X'YX4YX'X/X) X'YX'X-X*X1X'YY X) :- YX-X*X1Y X'X/X'X1X) X'YX*X:Y Y X1 **CCMP* X.YX'Y X'YYX*X1X) YY 18 b 20 YX(YYYYYYYYYYYX1X'Y X1 2024 *YYX/YX) YY X'YX/X'X1 X'YX9X1X(Y X) YYX*YYY X) X'YX'X/X'X1Y X) - **AHAD* X'YYX'YX1X) b X,YYYX1Y X) YX5X1 X'YX9X1X(Y X) YX9 X'YYX'YY X) X'YYX4X'X1YX) X'YY YX'Y Y X9X(X1 X2YY *X'YX4YX'X/X) YX9X*YX/X) X/YYY X'Y Y X-YYYY X'Y Y YX9X*X1Y X(YX' YY X,YY X9 X/YY X'YX9X'YY * *b" X*X5X/Y Y YX2X'X1X) X'YX.X'X1X,Y X) X'YYX5X1Y X) Y YYX*X( X'YX*X5X/Y YX'X* X'YYYX5YY * YX-X'YX1 X'YX(X1YX'YX,: X*X9X1Y Y X9X'Y X(X%X/X'X1X) X'YX*X:Y Y X1 YX#YYY X*Y YY X*X-YY Y X'YYYX'YX9. 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X'YX'X4X*X1X'Y YY YX0Y X'YYX,YYX9X) YX%Y YX'Y X*YYY X1X3X'X&Y X'YX%YYX*X1YYY X) YYYX'X X#X1X3Y X1X3X'YX) X%YYX*X1YYY X) X%YY ahadhrorg22+unsubscribe@googlegroups.com. YX9X1X6 YX0Y X'YYYX'YX4X) X9YY X'YYY X(X X'YX*YY X%YY https://groups.google.com/d/msgid/ahadhrorg22/CAEcxT4tQqiHYy5MMqsLJayryTMABYVLbdvZNvgx80Tc_0DvXKQ%40mail.gmail.com. ------------------------------ End of alt.music.moxy-fruvous digest V14 #13190 ***********************************************