From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #17030 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 Thursday, December 4 2025 Volume 14 : Number 17030 Today's Subjects: ----------------- Reverse Vitiligo Naturally ["Color Revival" ] Action Required: Delivery Exception Notification ["FedEx Support" Subject: Reverse Vitiligo Naturally Reverse Vitiligo Naturally http://skinviti.icu/QE5ua9R2-6b3QwETaiwEnHDvYX9t1FQy_lbaO4rvcq9rwjP-XQ http://skinviti.icu/ii73jib__Yxv5A5kiT5Xfv785df2MUq0QM8LedYh69Dj7W698w a is a large body of salt water. There are particular seas and the sea. The sea commonly refers to the ocean, the interconnected body of seawaters that spans most of Earth. Particular seas are either marginal seas, second-order sections of the oceanic sea (e.g. the Mediterranean Sea), or certain large, nearly landlocked bodies of water. The salinity of water bodies varies widely, being lower near the surface and the mouths of large rivers and higher in the depths of the ocean; however, the relative proportions of dissolved salts vary little across the oceans. The most abundant solid dissolved in seawater is sodium chloride. The water also contains salts of magnesium, calcium, potassium, and mercury, among other elements, some in minute concentrations. A wide variety of organisms, including bacteria, protists, algae, plants, fungi, and animals live in various marine habitats and ecosystems throughout the seas. These range vertically from the sunlit surface and shoreline to the great depths and pressures of the cold, dark abyssal zone, and in latitude from the cold waters under polar ice caps to the warm waters of coral reefs in tropical regions. Many of the major groups of organisms evolved in the sea and life may have started there. The ocean moderates Earth's climate and has important roles in the water, carbon, and nitrogen cycles. The surface of the water interacts with the atmosphere, exchanging properties such as particles and temperature, as well as currents. Surface currents are the water currents that are produced by the atmosphere's currents and its winds blowing over the surface of the water, producing wind waves, setting up through drag slow but stable circulations of water, as in the case of the ocean sustaining deep-sea ocean currents. Deep-sea currents, known together as the global conveyor belt, carry cold water from near the poles to every ocean and significantly influence Earth's climate. Tides, the generally twice-daily rise and fall of sea levels, are caused by Earth's rotation and the gravitational effects of the Moon and, to a lesser extent, of the Sun. Tides may have a very high range in bays or estuaries. Submarine earthquakes arising from tectonic plate movements under the oceans can lead to destructive tsunamis, as can volcanoes, huge landslides, or the impact of l ------------------------------ Date: Thu, 4 Dec 2025 10:55:46 +0100 From: "FedEx Support" Subject: Action Required: Delivery Exception Notification Action Required: Delivery Exception Notification http://flowenhance.space/sOGbDz2ko6b3gJF6n6dKn4Zht1-BJvddaJKbaoCNe_U9gFKvxg http://flowenhance.space/7LJtxUmceaf9yNdXPid-Xz8x0CKXZaha7GU-EtUHmgZ90V8jiQ r is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, areas where surface water eventually flows to a common outlet. Drainage divides keep rivers separated from other courses of water and causes upstream water within the confines of the divide to fall into the downhill stream. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape around it, forming deltas and islands where the flow slows down. Rivers rarely run in a straight line, instead, they bend or meander; the locations of a river's banks can change frequently. Rivers get their alluvium from erosion, which carves rock into canyons and valleys. Rivers have sustained human and animal life for millennia, including the first human civilizations. The organisms that live around or in a river such as fish, aquatic plants, and insects have different roles, including processing organic matter and predation. Rivers have produced abundant resources for humans, including food, transportation, drinking water, and recreation. Humans have engineered rivers to prevent flooding, irrigate crops, perform work with water wheels, and produce hydroelectricity from dams. People associate rivers with life and fertility and have strong religious, political, social, and mythological attachments to them. Rivers and river ecosystems are threatened by water pollution, climate change, and human activity. The construction of dams, canals, levees, and other engineered structures has eliminated habitats, has caused the extinction of some species, and lowered the amount of alluvium flowing through rivers. Decreased snowfall from climate change has resulted in less water available for rivers during the summer. Regulation of pollution, dam removal, and sewage treatment have helped to improve water quality and restore river hab ------------------------------ Date: Thu, 4 Dec 2025 07:42:13 -0600 From: "CVS Member Gift" Subject: Today Only: Free Gift from CVS Today Only: Free Gift from CVS http://careqik.icu/uzrvBNCvStGDZGcA9Txm_s8j3ySbelodccBMldWyJWdg7cUO http://careqik.icu/SmL8RW92GksNwwzDqeO8aTLFi1UTgkLVH9Skeh0JxPu_qdp9FA harus is either an osmoconformer or a weak osmoregulator. It can reverse the direction of its ventilatory flow by adjusting the sizes of apertures located at the bases of its legs, presumed to be a means of keeping particulate matter from obstructing these apertures. The apertures lead into the branchial chamber and are covered in dense setae for filtration. Unlike in most decapods, this period of reversed flow can be sustained, and it is commonly seen when the crab is buried or at rest. Its heart is a single-chambered ventricle which ejects hemolymph to seven arteries. Five arteries, including the anterior aorta, leave the heart anteriorly and supply organs such as the cerebral ganglion, eyes, antennae, hepatopancreas, and various digestive organs. One, which leaves the heart ventrally, is called the sternal artery and accounts for nearly 70% of flow; this branches into vessels which supply its five pairs of legs, the largest of which are those supplying its rear paddles. Finally, a relatively small posterior aorta runs down the middle of the crab's abdomen. Ovalipes catharus is a stenotherm, highly sensitive to temperature. An increase in water temperature of just a few degrees substantially accelerates its growth. At summer temperatures of about , catharus' heart rate is approximately 50 bpm. Above this temperature, its heartbeats begin to shorten. Its heart rate is more than doubled to 125 bpm at 25 B0C (77 B0F), and temperatures around 30 B0C (86 B0F) are fatal. Phosphorylation of ADP during respiration also decreases at temperatures over 20 B0C (68 B0F), indicating reduced ability of the mitochondria to produce ATP. At temperatures around 10 B0C (50 B0F) b near the lower end of what it experiences in the wild.. catharus needs to be actively encouraged to eat, eats less overall, and takes over three times as long to digest its food as it does at . Ovalipes catharus hears underwater by using a small canal system located under its first antenna called a statocyst. The statocyst contains an agglomerate of sand particles called the statolith and functions similarly to the otolith in vertebrates. O. cath ------------------------------ Date: Thu, 4 Dec 2025 03:39:20 -0600 From: "The Star Shower Team" Subject: Looking For An Innovative Way To Decorate Your Home This Holiday Looking For An Innovative Way To Decorate Your Home This Holiday http://heatwellnow.space/x2v7Xg8mpfG6rjIfZKAgkYH2bf1qVFii61qORBDJB24oIcehhg http://heatwellnow.space/tyomB51DHshlRH3imYrYKxuJQAvQTcqmdR9BV0GPOux-TDZ4Tw er is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, areas where surface water eventually flows to a common outlet. Drainage divides keep rivers separated from other courses of water and causes upstream water within the confines of the divide to fall into the downhill stream. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape around it, forming deltas and islands where the flow slows down. Rivers rarely run in a straight line, instead, they bend or meander; the locations of a river's banks can change frequently. Rivers get their alluvium from erosion, which carves rock into canyons and valleys. Rivers have sustained human and animal life for millennia, including the first human civilizations. The organisms that live around or in a river such as fish, aquatic plants, and inse ------------------------------ Date: Thu, 4 Dec 2025 15:25:02 +0100 From: "Health Plans America" Subject: Are you eligible for a Health insurance Plan? Are you eligible for a Health insurance Plan? http://grainstone.help/YTLcvrRXvQiKv8C_gBJqzInCdNNdRVEpWNLcoZZiAhYS9l5m http://grainstone.help/XLDhH6PUlGFN5IhojOD-Oi6DPv7PlC2OUr68aWIy1wv0fRQg_A vers are part of the water cycle, the continuous processes by which water moves about Earth. This means that all water that flows in rivers must ultimately come from precipitation. The sides of rivers have land that is at a higher elevation than the river itself, and in these areas, water flows downhill into the river. The headwaters of a river are the smaller streams that feed a river, and make up the river's source. These streams may be small and flow rapidly down the sides of mountains. All of the land uphill of a river that feeds it with water in this way is in that river's drainage basin or watershed. A ridge of higher elevation land is what typically separates drainage basins; water on one side of a ridge will flow into one set of rivers, and water on the other side will flow into another. One example of this is the Continental Divide of the Americas in the Rocky Mountains. Water on the western side of the divide flows into the Pacific Ocean, whereas water on the other side flows into the Atlantic Ocean. The end of a glacier, which looks like a wall of ice. Blue water filled with snow and ice is at the bottom of the cliff. Melting toe of the Perito Moreno Glacier in Los Glaciares National Park, Argentina Not all precipitation flows directly into rivers; some water seeps into underground aquifers. These, in turn, can still feed rivers via the water table, the groundwater beneath the surface of the land stored in the soil. Water flows into rivers in places where the river's elevation is lower than that of the water table. This phenomenon is why rivers can still flow even during times of drought. Rivers are also fed by the melting of snow glaciers present in higher elevation regions. In summer months, higher temperatures melt snow and ice, causing additional water to flow into rivers. Glacier melt can supplement snow melt in times like the late summer, when there may be less snow left to melt, helping to ensure that the rive ------------------------------ End of alt.music.moxy-fruvous digest V14 #17030 ***********************************************