From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #14098 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 Friday, June 14 2024 Volume 14 : Number 14098 Today's Subjects: ----------------- Non-Stick Pan Can Cook Nearly Anything! ["Quality Cookware" Subject: Non-Stick Pan Can Cook Nearly Anything! Non-Stick Pan Can Cook Nearly Anything! http://ketobreadsdesserts.ru.com/QKV2WGdKGZL-blahGAR2RXr4_qZndAS42Ma5jNsYPP8rjBZorg http://ketobreadsdesserts.ru.com/nGVOGrdk8fPfAsXAQlykTusfGRQy3JpccnRgmOgXuSZqB-QGGg ue to Earth's rotation it has the shape of an ellipsoid, bulging at its Equator; its diameter is 43 kilometers (27 mi) longer there than at its poles. Earth's shape furthermore has local topographic variations. Though the largest local variations, like the Mariana Trench (10,925 meters or 35,843 feet below local sea level), only shortens Earth's average radius by 0.17% and Mount Everest (8,848 meters or 29,029 feet above local sea level) lengthens it by only 0.14%.[n 6] Since Earth's surface is farthest out from Earth's center of mass at its equatorial bulge, the summit of the volcano Chimborazo in Ecuador (6,384.4 km or 3,967.1 mi) is its farthest point out. Parallel to the rigid land topography the Ocean exhibits a more dynamic topography. To measure the local variation of Earth's topography, geodesy employs an idealized Earth producing a shape called a geoid. Such a geoid shape is gained if the ocean is idealized, covering Earth completely and without any perturbations such as tides and winds. The result is a smooth but gravitational irregular geoid surface, providing a mean sea level (MSL) as a reference level for topographic measurements. Surface Further information: Planetary surface, Land cover, Land, Pedosphere, Ocean, Sea, Cryosphere, and Peplosphere A composite image of Earth, with its different types of surface discernible: Earth's surface dominating Ocean (blue), Africa with lush (green) to dry (brown) land and Earth's polar ice in the form of Antarctic sea ice (grey) covering the Antarctic or Southern Ocean and the Antarctic ice sheet (white) covering Antarctica. Relief of Earth's crust Earth's surface is the boundary between the atmosphere, and the solid Earth and oceans. Defined in this way, it has an area of about 510 million km2 (197 million sq mi). Earth can be divided into two hemispheres: by latitude into the polar Northern and Southern hemispheres; or by longitude into the continental Eastern and Western hemispheres. Most of Earth's surface is ocean water: 70.8% or 361 million km2 (139 million sq mi). This vast pool of salty water is often called the world oce ------------------------------ Date: Thu, 13 Jun 2024 12:34:21 +0200 From: "Translator" Subject: Order Now To Get A Special 5O% OFF Order Now To Get A Special 5O% OFF http://boostaroplus.info/sA-SZoiRZiSqYHhAqIIntCJRSy2ldS5Um8Ls1d4EbuX3YKgkdQ http://boostaroplus.info/ImbQcSnP3wqKrQcPUiinfTt6-Rt2YdHyiG_-mcqASdC9-YaP4Q esis has been termed "Snowball Earth", and it is of particular interest because it preceded the Cambrian explosion, when multicellular life forms significantly increased in complexity. Following the Cambrian explosion, 535 Ma, there have been at least five major mass extinctions and many minor ones. Apart from the proposed current Holocene extinction event, the most recent was 66 Ma, when an asteroid impact triggered the extinction of non-avian dinosaurs and other large reptiles, but largely spared small animals such as insects, mammals, lizards and birds. Mammalian life has diversified over the past 66 Mys, and several million years ago, an African ape species gained the ability to stand upright. This facilitated tool use and encouraged communication that provided the nutrition and stimulation needed for a larger brain, which led to the evolution of humans. The development of agriculture, and then civilization, led to humans having an influence on Earth and the nature and quantity of other life forms that continues to this day. Future Main article: Future of Earth See also: Global catastrophic risk A dark gray and red sphere representing the Earth lies against a black background to the right of an orange circular object representing the Sun Conjectured illustration of the scorched Earth after the Sun has entered the red giant phase, about 5b7 billion years from now Earth's expected long-term future is tied to that of the Sun. Over the next 1.1 billion years, solar luminosity will increase by 10%, and over the next 3.5 billion years by 40%. Earth's increasing surface temperature will accelerate the inorganic carbon cycle, reducing CO2 concentration to levels lethally low for plants (10 ppm for C4 photosynthesis) in approximately 100b900 million years. The lack of vegetation will result in the loss of oxygen in the atmosphere, making animal life impossible. Due to the increased luminosity, Earth's mean temperature may reach 100 B0C (212 B0F) in 1.5 billion years, and all ocean water will evaporate and be lost to space, which may trigger a runaway greenhouse effect, within an estimated 1.6 to 3 billion years. Even if the Sun were stable, a fraction of the water in the modern oceans will descend to the mantle, due to reduced steam venting from mid-ocean ridges. The Sun will evolve to become a red giant in about 5 billion years. Models predict that the Sun will expand to roughly 1 AU (150 million km; 93 million mi), about 250 times its present radius. Earth's fate is less clear. As a red giant, the Sun will lose roughly 30% of its mass, so, without tidal effects, Earth will move to an orbit 1.7 AU (250 million km; 160 million mi) from the Sun when the star reaches its maximum radius, other ------------------------------ Date: Thu, 13 Jun 2024 15:11:49 +0200 From: "Weight loss" Subject: Lose over 20% of Lose Up To 20% of Body Weight with GLP-1s1 Lose over 20% of Lose Up To 20% of Body Weight with GLP-1s1 http://horizonsacehard.za.com/Zzwl0sNLon1FxgmYW3DW6zQ55nTqC7JgrVb1Q16ZNJ9LLJk http://horizonsacehard.za.com/1wl6x3Jtd6C_aO5i5tmO_ZXCtPokgJVjGsr6IVoCeJLa14LaVQ nd can be covered by surface water, snow, ice, artificial structures or vegetation. Most of Earth's land hosts vegetation, but considerable amounts of land are ice sheets (10%, not including the equally large area of land under permafrost) or deserts (33%) The pedosphere is the outermost layer of Earth's land surface and is composed of soil and subject to soil formation processes. Soil is crucial for land to be arable. Earth's total arable land is 10.7% of the land surface, with 1.3% being permanent cropland. Earth has an estimated 16.7 million km2 (6.4 million sq mi) of cropland and 33.5 million km2 (12.9 million sq mi) of pastureland. The land surface and the ocean floor form the top of Earth's crust, which together with parts of the upper mantle form Earth's lithosphere. Earth's crust may be divided into oceanic and continental crust. Beneath the ocean-floor sediments, the oceanic crust is predominantly basaltic, while the continental crust may include lower density materials such as granite, sediments and metamorphic rocks. Nearly 75% of the continental surfaces are covered by sedimentary rocks, although they form about 5% of the mass of the crust. Earth's surface topography comprises both the topography of the ocean surface, and the shape of Earth's land surface. The submarine terrain of the ocean floor has an average bathymetric depth of 4 km, and is as varied as the terrain above sea level. Earth's surface is continually being shaped by internal plate tectonic processes including earthquakes and volcanism; by weathering and erosion driven by ice, water, wind and temperature; and by biological processes including the growth and decomposition of biomass into soil. Tectonic plates Main article: Plate tectonics Shows the extent and boundaries of tectonic plates, with superimposed outlines of the continents they support Earth's major plates, which are: Pacific Plate African Plate[n 7] North American Plate Eurasian Plate Antarctic Plate Indo-Australian Plate South American Plate Earth's mechanically rigid outer layer of Earth's crust and upper mantle, the lithosphere, is divided into tectonic plates. These plates are rigid segments that move relative to each other at one of three boundaries types: at convergent boundaries, two plates come together; at divergent boundaries, two plates are pulled apart; and at transform boundaries, two plates slide past one another laterally. Along these plate boundaries, earthquakes, volcanic activity, mountain-building, and oceanic trench formation can occur. The tectonic plates ride on top of the asthenosphere, the solid but less-viscous part of the upper mantle that can flow ------------------------------ Date: Thu, 13 Jun 2024 12:29:31 +0200 From: "Last Minute Giveaway" Subject: Lucky chance to receive a FREE Target Stanley Cup Lucky chance to receive a FREE Target Stanley Cup http://fatburnkitchen.za.com/zK083sqnOV7ePg_ExcDrGappEwiuntjVQ7I09iVgD1uq0NQ12Q http://fatburnkitchen.za.com/C8AHugc39jwhQ161qgGNFooKD19EIJdAPViyrVy4JG_DtRX5Mg e Last Glacial Period, colloquially called the "last ice age", covered large parts of the continents, to the middle latitudes, in ice and ended about 11,700 years ago. Origin of life and evolution Main articles: Origin of life, Earliest known life forms, and History of life Chemical reactions led to the first self-replicating molecules about four billion years ago. A half billion years later, the last common ancestor of all current life arose. The evolution of photosynthesis allowed the Sun's energy to be harvested directly by life forms. The resultant molecular oxygen (O2) accumulated in the atmosphere and due to interaction with ultraviolet solar radiation, formed a protective ozone layer (O3) in the upper atmosphere. The incorporation of smaller cells within larger ones resulted in the development of complex cells called eukaryotes. True multicellular organisms formed as cells within colonies became increasingly specialized. Aided by the absorption of harmful ultraviolet radiation by the ozone layer, life colonized Earth's surface. Among the earliest fossil evidence for life is microbial mat fossils found in 3.48 billion-year-old sandstone in Western Australia, biogenic graphite found in 3.7 billion-year-old metasedimentary rocks in Western Greenland, and remains of biotic material found in 4.1 billion-year-old rocks in Western Australia. The earliest direct evidence of life on Earth is contained in 3.45 billion-year-old Australian rocks showing fossils of microorganisms. An artist's impression of the Archean, the eon after Earth's formation, featuring round stromatolites, which are early oxygen-producing forms of life from billions of years ago. After the Late Heavy Bombardment, Earth's crust had cooled, its water-rich barren surface is marked by continents and volcanoes, with the Moon still orbiting Earth half as far as it is today, appearing 2.8 times larger and producing strong tides. During the Neoproterozoic, 1000 to 539 Ma, much of Earth might have been covere ------------------------------ Date: Thu, 13 Jun 2024 16:18:12 +0200 From: "Tractor Supply Rewards" Subject: Lucky chance to receive a FREE HART Cordless 6-Tool Combo Kit Lucky chance to receive a FREE HART Cordless 6-Tool Combo Kit http://purpleburnpros.co.uk/cm6UyXknt-nLp8CdXclnmoM6QAfSvIVhxyf0L4jHfVRgxhB8DA http://purpleburnpros.co.uk/tHORvaH76fmaFT_czcoGl5u0GJSHAgQvXXfsfDv4HN6wocuFPA eath the lithosphere is the asthenosphere, a relatively low-viscosity layer on which the lithosphere rides. Important changes in crystal structure within the mantle occur at 410 and 660 km (250 and 410 mi) below the surface, spanning a transition zone that separates the upper and lower mantle. Beneath the mantle, an extremely low viscosity liquid outer core lies above a solid inner core. Earth's inner core may be rotating at a slightly higher angular velocity than the remainder of the planet, advancing by 0.1b0.5B0 per year, although both somewhat higher and much lower rates have also been proposed. The radius of the inner core is about one-fifth of that of Earth. The density increases with depth. Among the Solar System's planetary-sized objects, Earth is the object with the highest density. Chemical composition Further information: Abundance of the chemical elements B' Earth See also: Abundance of elements in Earth's crust Earth's mass is approximately 5.97C1024 kg (5,970 Yg). It is composed mostly of iron (32.1% by mass), oxygen (30.1%), silicon (15.1%), magnesium (13.9%), sulfur (2.9%), nickel (1.8%), calcium (1.5%), and aluminium (1.4%), with the remaining 1.2% consisting of trace amounts of other elements. Due to gravitational separation, the core is primarily composed of the denser elements: iron (88.8%), with smaller amounts of nickel (5.8%), sulfur (4.5%), and less than 1% trace elements. The most common rock constituents of the crust are oxides. Over 99% of the crust is composed of various oxides of eleven elements, principally oxides containing silicon (the silicate minerals), aluminium, iron, calcium, magnesium, potassium, or sodiu ------------------------------ End of alt.music.moxy-fruvous digest V14 #14098 ***********************************************