From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #16166 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, June 9 2025 Volume 14 : Number 16166 Today's Subjects: ----------------- Hurry up ! You are the recipient of Blackstone Original 4-Burner ["Costco] Approved by Harvard ["Tinnitus GONE" ] You have won an CVS Pharmacy Oral-B 9 ["CVS Pharmacy" Subject: Hurry up ! You are the recipient of Blackstone Original 4-Burner Hurry up ! You are the recipient of Blackstone Original 4-Burner http://savageplus.za.com/usS6Z1EHsYEK0TyZJGYDVQc_CimV-M3KUI-5ZS6uvQGguBUIwg http://savageplus.za.com/YJ2S8uBydXBbbhM9UM8AxTJOitwUEOy0aItC16mwuY7b_xEZLQ ddle and Late Devonian rocks, known as Ilfracombe beds and Morte Slates. These include sandstone and limestone, which have been quarried near Aisholt. At Great Holwell, south of Aisholt, is the only limestone cave in the Devonian limestone of North Devon and West Somerset. The lower fringes around the hills are composed of younger New Red Sandstone rocks of the Triassic period. These rocks were laid down in a shallow sea and often contain irregular masses or veins of gypsum, which was mined on the foreshore at Watchet. Several areas have outcrops of slates. Younger rocks of the Jurassic period can be found between St Audries and Kilve. This area falls within the Blue Anchor to Lilstock Site of Special Scientific Interest (SSSI) and is considered to be of international geological importance. Kilve has the remains of a red-brick retort built in 1924 after the shale in the cliffs was found to be rich in oil. Along this coast, the cliffs are layered with compressed strata of oil-bearing shale and blue, yellow and brown Lias embedded with fossils. The Shaline Company was founded in 1924 to exploit these strata but was unable to raise sufficient capital. The company's retort house is thought to be the first structure erected here for the conversion of shale to oil and is all that remains of the anticipated Somerset oil boom. At Blue Anchor the coloured alabaster found in the cliffs gave rise to the name of the colour "Watchet Blue". The village has the only updraught brick kiln known to have survive ------------------------------ Date: Sun, 8 Jun 2025 08:43:53 +0200 From: "Tinnitus GONE" Subject: Approved by Harvard Approved by Harvard http://cardiansafecard.click/4uFHpo6zzTQobWDXX4SPDw5QG2s-lI5kV18CkEHEjlBL77fzQA http://cardiansafecard.click/L54etJmRtPjsJRTSwstFzFnzR8rzfxr0xT3qPbCd9wlm33-qHA anges in sea level relative to a fixed point, such as the centre of the earth, for example as a result of melting ice-caps. "steric" refers to global changes in sea level due to thermal expansion and salinity variations. "isostatic" refers to changes in the level of the land relative to a fixed point in the earth, possibly due to thermal buoyancy or tectonic effects, disregarding changes in the volume of water in the oceans. The melting of glaciers at the end of ice ages results in isostatic post-glacial rebound, when land rises after the weight of ice is removed. Conversely, older volcanic islands experience relative sea level rise, due to isostatic subsidence from the weight of cooling volcanos. The subsidence of land due to the withdrawal of groundwater is another isostatic cause of relative sea level rise. On planets that lack a liquid ocean, planetologists can calculate a "mean altitude" by averaging the heights of all points on the surface. This altitude, sometimes referred to as a "sea level" or zero-level elevation, serves equivalently as a reference for the height of planetary featur ------------------------------ Date: Sat, 7 Jun 2025 20:32:09 -0500 From: "CVS Pharmacy" Subject: You have won an CVS Pharmacy Oral-B 9 You have won an CVS Pharmacy Oral-B 9 http://activator.ru.com/ph6E3KFoxcE0zUTxo6zEyJu7oPrRmiPSdyGeiketaf_9K7UH http://activator.ru.com/n6NyRV3dfW7kSw1oJmlHewMm7oB3cGW10fUcSXhawoOrh1Zl ands emerge from the deep abyss of the ocean, and feature rough or mountainous landscapes in their interiors and a diverse array of summit elevations. Researchers have observed that the island will often be covered by dense tropical forest. These limit settlement on the interior of many islands, forcing communities to develop along the coast. Larger islands may have rivers, resulting in flood hazards. Rivers deliver sediment downstream, which can dominate the shape of the coast and contribute to erosion. Tall volcanic islands are often surrounded by protective fringing or barrier reefs, creating lagoons. The unique geological and geographical characteristics of volcanic islands make them prone to many natural hazards, which are expected to worsen due to climate change. These inclu ------------------------------ Date: Sat, 7 Jun 2025 12:50:26 -0500 From: "Aging Fix" Subject: Try THIS "anti-aging" trick (adds 13 years to lifespan?) Try THIS "anti-aging" trick (adds 13 years to lifespan?) http://spectrelaptop.ru.com/hPwpx1qpsDYYBkklnSRSH_BeoJjojDT0xlcy7DwrmyzYYgbt http://spectrelaptop.ru.com/NZs9zGgd2nwBzLYNtVlC4ctsgBPEM8hJB5PIBFrzn3p0JJ2W awater precipitate high-magnesium calcite instead. This substance, which has an excess of calcium over magnesium and lacks calcium-magnesium ordering, is sometimes called protodolomite. Raising the temperature makes it easier for magnesium to shed its hydration shell, and dolomite can be precipitated from seawater at temperatures in excess of 60 B0C (140 B0F). Protodolomite also rapidly converts to dolomite at temperatures of 250 B0C (482 B0F) or higher. The high temperatures necessary for the formation of dolomite helps explain the rarity of Cenozoic dolomites, since Cenozoic seawater temperatures seldom exceeded 40 B0C. It is possible that microorganisms are capable of precipitating primary dolomite. This was first demonstrated in samples collected at Lagoa Vermelha, Brazil in association with sulfate-reducing bacteria (Desulfovibrio), leading to the hypothesis that sulfate ion inhibits dolomite nucleation. Later laboratory experiments suggest bacteria can precipitate dolomite independently of the sulfate concentration. With time other pathways of interaction between microbial activity and dolomite formation have been added to the discord regarding their role in modulation and generation of polysaccharides, manganese and zinc within the porewater. Meanwhile, a contrary view held by other researchers is that microorganisms precipitate only high-magnesium calcite but leave open the question of whether this can lead to precipitation of dolom ------------------------------ Date: Sat, 7 Jun 2025 17:38:22 -0500 From: "Trump Decanter Set" Subject: This Decanter Set Was Made for Legends Like Him This Decanter Set Was Made for Legends Like Him http://wildguide.ru.com/iVP4-UgwHerd_XiR8tnBgG5WoYoZU-QCg_iQcTPkdl18WDdH http://wildguide.ru.com/s-jqsfb3DtVpm0Jtpj1L0JaqpovO6-nQrVhKiEiIBG3MY6M molish, while property south of the river contained slums and cheap property, making it easier to have terminal stations close to the City and West End, both the main desired areas. The solicitor and railway planner Charles Pearson proposed a main central station at Farringdon, which would connect out to all branch lines. In 1846, the Royal Commission on Metropolitan Railway Termini was established to see if it was appropriate to bring the terminal stations any further and possibly connect with each other, as per Pearson's plans. The report concluded this was unnecessary, a single terminal was undesirable as it would create too much congestion and it was too expensive to demolish remaining property in the way. The Royal Commission recommended that no new stations should be built in the West End of London or the city, and that the New Road should be the northern boundary of railway development. This created competition between the individual railway companies, who could promote new terminals with individual financial backers. Exemptions were made for the Great Eastern Railway and North London Railway with Liverpool Street and Broad Street respectively. The only main railway line built across Central London was the London, Chatham and Dover Railway (LCDR) line connecting Blackfriars to Farringdon via Snow Hill Tunn ------------------------------ Date: Sat, 7 Jun 2025 18:45:05 +0200 From: "Ancient Relief" Subject: Say Goodbye to Painkillers Say Goodbye to Painkillers http://nicoyapuretea.click/NKEkNHTjggWO6yc_7mJMGf6qgKoaF1pZKbV6ruU3TxldTIW7JQ http://nicoyapuretea.click/ADaKuu12Sg8eyLQnF7FfAg1jMZ3GhDCYLlLTOEtHa-pPxb9hVA aracterized by its nearly ideal 1:1 stoichiometric ratio of magnesium to calcium. It is distinct from high-magnesium limestone in that the magnesium and calcium form ordered layers within the individual dolomite mineral grains, rather than being arranged at random, as they are in high-magnesium calcite grains. In natural dolomite, magnesium is typically between 44 and 50 percent of total magnesium plus calcium, indicating some substitution of calcium into the magnesium layers. A small amount of ferrous iron typically substitutes for magnesium, particularly in more ancient dolomites. Carbonate rock tends to be either almost all calcite or almost all dolomite, with intermediate compositions being quite uncommon. Dolomite outcrops are recognized in the field by their softness (mineral dolomite has a Mohs hardness of 4 or less, well below common silicate minerals) and because dolomite bubbles feebly when a drop of dilute hydrochloric acid is dropped on it. This distinguishes dolomite from limestone, which is also soft but reacts vigorously with dilute hydrochloric acid. Dolomite usually weathers to a characteristic dull yellow-brown color due to the presence of ferrous iron. This is released and oxidized as the dolomite weathers. Dolomite is usually granular in appearance, with a texture resembling grains of sugar. Under the microscope, thin sections of dolomite usually show indiv ------------------------------ Date: Sat, 7 Jun 2025 19:15:31 -0500 From: "Omaha Steaks Customer Support" Subject: Your chance to receive a FREE Omaha Steaks Kit Your chance to receive a FREE Omaha Steaks Kit http://wildguide.ru.com/d1b0LiKS75_Azwh2qKc_rd1fgn9fytZdCDjir5UxEEG0HLy4 http://wildguide.ru.com/kDgZ5fKYvn5yeLmw_S75-ZgJqhZQeiiBPTUVpA7snPNJ1lki ons were developed in the mid-19th century during the initial boom of rail transport. Many stations were built around the edge of central London, stopping at what is now the London Inner Ring Road, because it was prohibitively expensive to build right into the centre, and because each railway was owned by a private company competing with the others. The creation of the London Underground provided a practical connection to the various terminals, which continues to be the case as of the 21st century. Many of the stations have been upgraded and modernised to provide a greater capacity and connections to the network; the first London terminal, London Bridge has been rebuilt and expanded on numerous occasions, and of the major 19th century terminals, only Broad Street and Holborn Viaduct have closed. The latter was replaced by the nearby City Thameslink. The London terminals had a significant impact on the local area. Originally, the demolition of poor properties, particularly south of the River Thames, caused blight and deprived areas around the station. This has changed in the 21st century, where development around the main terminals has been well-received and attracted occu ------------------------------ Date: Sun, 8 Jun 2025 10:24:18 +0200 From: "Horsepower Duck Affiliates" Subject: Get Turbocharged Cleaning Power - Up to 50% OFF! 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Refinements were also made following early flight testing to the rudder and elevator to reduce instances of buffeting, after which it is claimed that the Canberra handled much like a fighter, proving to be atypically manoeu ------------------------------ Date: Sat, 7 Jun 2025 14:15:38 -0500 From: "Plant Power" Subject: Yard Weed Hiding Ancient Medicinal Power Yard Weed Hiding Ancient Medicinal Power http://vitrafoxin.click/o_HP6ky10ZuJjHZvyhI1N7MGi-MwXEqYO1qq6BPdqXdZEEZ0 http://vitrafoxin.click/6qS2ghL7FeSUN5gVoBa1A2bHBVZ7LuwnlHd77i4pzdrGvzVY erizing deeper burial, if a mechanism exists to flush magnesium-bearing fluids through the beds. Mineral dolomite has a 12% to 13% smaller volume than calcite per alkali cation. Thus dolomitization likely increases porosity and contributes to the sugary texture of dolomite. The dolomite problem and primary dolomite Dolomite is supersaturated in normal seawater by a factor of greater than ten, but dolomite is not seen to precipitate in the oceans. Likewise, geologists have not been successful at precipitating dolomite from seawater at normal temperatures and pressures in laboratory experiments. This is likely due to a very high activation energy for nucleating crystals of dolomite. The magnesium ion is a relatively small ion, and it acquires a tightly bound hydration shell when dissolved in water. In other words, the magnesium ion is surrounded by a clump of water molecules that are strongly attracted to its positive charge. Calcium is a larger ion and this reduces the strength of binding of its hydration shell, so it is much easier for a calcium ion than a magnesium ion to shed its hydration shell and bind to a growing crystal. It is also more difficult to nucleate a seed crystal of ordered dolomite than disordered hi ------------------------------ Date: Sat, 7 Jun 2025 11:36:17 -0500 From: "Forbidden Brain Science" Subject: Your memory is dying (unless you do THIS) Your memory is dying (unless you do THIS) http://healthcareseries.sa.com/y0EhXDo66yepKO8YgK136brGerj0VCTzf8U69874HHfaHbu9 http://healthcareseries.sa.com/92l5gwiRpPgKCzwQQbpPXNUs3N7VPoLaY_IEZ8RQwBm7XqhY an also, less commonly, form through dissolution of rock by sulfuric acid. Calcium carbonate speleothems (secondary deposits) in the forms of stalactites, stalagmites, flowstone etc., can also form in caves within dolomite rock. bDolomite is a common rock type, but a relatively uncommon mineral in speleothemsb. Both the 'Union Internationale de SpC)lC)ologie' (UIS) and the American 'National Speleological Society' (NSS), extensively use in their publications, the terms "dolomite" or "dolomite rock" when referring to the natural bedrock containing a high percentage of CaMg(CO3)2 in which natural caves or solution tubes have formed. Dolomite speleothems Both calcium and magnesium go into solution when dolomite rock is dissolved. The speleothem precipitation sequence is: calcite, Mg-calcite, aragonite, huntite and hydromagnesite. Hence, the most common speleothem (secondary deposit) in caves within dolomite rock karst, is calcium carbonate in the most stable polymorph form of calcite. Speleothem types known to have a dolomite constituent include: coatings, crusts, moonmilk, flowstone, coralloids, powder, spar and rafts. 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