From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #3961 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 Monday, April 13 2020 Volume 14 : Number 3961 Today's Subjects: ----------------- This strange device will start a huge scandal ["Easy Power Plan" Subject: This strange device will start a huge scandal This strange device will start a huge scandal http://sqribbmass.bid/gpzDLZQ6jpJQT90uNKZ-ZN0LznwKxgJxSUgM62b0d_I7LjQ http://sqribbmass.bid/_cIMd1A332f37XkTtl4n515QyzzXklHxZQ7U4xjxoDrnpCS- Although the Sun dominates the system by mass, it accounts for only about 2% of the angular momentum. The planets, dominated by Jupiter, account for most of the rest of the angular momentum due to the combination of their mass, orbit, and distance from the Sun, with a possibly significant contribution from comets. The Sun, which comprises nearly all the matter in the Solar System, is composed of roughly 98% hydrogen and helium. Jupiter and Saturn, which comprise nearly all the remaining matter, are also primarily composed of hydrogen and helium. A composition gradient exists in the Solar System, created by heat and light pressure from the Sun; those objects closer to the Sun, which are more affected by heat and light pressure, are composed of elements with high melting points. Objects farther from the Sun are composed largely of materials with lower melting points. The boundary in the Solar System beyond which those volatile substances could condense is known as the frost line, and it lies at roughly 5 AU from the Sun. The objects of the inner Solar System are composed mostly of rock, the collective name for compounds with high melting points, such as silicates, iron or nickel, that remained solid under almost all conditions in the protoplanetary nebula. Jupiter and Saturn are composed mainly of gases, the astronomical term for materials with extremely low melting points and high vapour pressure, such as hydrogen, helium, and neon, which were always in the gaseous phase in the nebula. Ices, like water, methane, ammonia, hydrogen sulfide, and carbon dioxide, have melting points up to a few hundred kelvins. They can be found as ices, liquids, or gases in various places in the Solar System, whereas in the nebula they were either in the solid or gaseous phase. Icy substances comprise the majority of the satellites of the giant planets, as well as most of Uranus and Neptune (the so-called "ice giants") and the numerous small objects that lie beyond Neptune's orbit. Together, gases and ices are referred ------------------------------ Date: Sun, 12 Apr 2020 12:41:18 -0400 From: "Sanitize Your Household" Subject: No-Contact Multi-Fnctional Digital Thermometer No-Contact Multi-Fnctional Digital Thermometer http://bloodpressupl.co/qhdnTPs559Yhd1-zMLnoKYTYKc2PSlphz-YDEQ70i1-Axjwj http://bloodpressupl.co/qhIQ_FEdL_tDpVw96aLbN5aCG4lygUpVKyc8JD7IcjIBGo8v arliest thrusts of the Sevier are located furthest west with each newer thrust cutting the older thrust. This pattern caused the older thrusts to ride on top of the younger thrusts as they moved eastward. The Paris-Willard thrust in Utah was determined to be the oldest thrust in the series using this pattern. The youngest thrust is the Hogback in Wyoming. The Sevier thrust belt in Utah can be divided in two, north of Salt Lake City and South of Salt Lake City. The thrusts to the north are much better understood because oil and gas are often associated with them. The northern portion runs through present day Utah, Idaho, and Wyoming. The southern portion stops around Las Vegas. The total crustal shortening of the northern portion was roughly 60 miles. This is a diagram showing how transverse zones often connect thrust faults in a fold and thrust belt. The Sevier belt left behind many distinctive geologic features in the Wyoming and Utah region, namely recesses and salients. Transverse zones can accompany thrust faults connecting the segments of the belt. One such zone is the Charleston transverse zone linking the Provo salient to the southern arm of the Uinta/Cottonwood arch. Although the Uinta/Cottonwood arch is a Laramide structure the Sevier helped the arch form. Another important zone is the Mount Raymond transverse zone connecting the Wyoming salient and the northern arm of the arch. While continental margins are typically the most deformed in orogenic events, the interior of continental plates can also deform. In the Sevier-Laramide orogenic events evidence for interior plate deformation includes folds, cleavage and joint fabrics, distorted fossils, persistent faulting, and calcite twinning. This is a cross section of the Sevier fold and thrust belt along with major geologic features that accompanied the orogeny. How and when The Sevier fold and thrust belt was active between late Jurassic through Eocene time. The actual age of initiation of the belt is not entirely agreed upon by researchers. The beginning of deformation in the earliest stages of the orogeny started about 120-80 Ma (millions of years ago) with the formation and continuation of a magmatic arc and foreland fold-thrust belt. However, data from the southern portion of the belt shows contraction in southern Nevada and southeastern California beginning about 200 to 92 Ma largely based on intrusions and the formation of the Lavinia Wa ------------------------------ End of alt.music.moxy-fruvous digest V14 #3961 **********************************************