From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #13753 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 Saturday, April 20 2024 Volume 14 : Number 13753 Today's Subjects: ----------------- Asian Sex Cult Penis Ritual Leaked (Disturbing Video) ["Asian Sex" Subject: Asian Sex Cult Penis Ritual Leaked (Disturbing Video) Asian Sex Cult Penis Ritual Leaked (Disturbing Video) http://aizenpowers.ru.com/sNMsZ3yDwxk6Ud6JEaXSeLEa8agVueRR5KkeFpPudLkmh_AbhA http://aizenpowers.ru.com/p07LjsOm8Nbj1hTFEVOmDh_TQzM9CyHTDotjAAC-cJBafTToqA was designed by Irish-born architect James Hoban in the Neoclassical style. Hoban modeled the building on Leinster House in Dublin, a building which today houses the Oireachtas, the Irish legislature. Construction took place between 1792 and 1800, with an exterior of Aquia Creek sandstone painted white. When Thomas Jefferson moved into the house in 1801, he and architect Benjamin Henry Latrobe added low colonnades on each wing to conceal what then were stables and storage. In 1814, during the War of 1812, the mansion was set ablaze by British forces in the burning of Washington, destroying the interior and charring much of the exterior. Reconstruction began almost immediately, and President James Monroe moved into the partially reconstructed Executive Residence in October 1817. Exterior construction continued with the addition of the semicircular South Portico in 1824 and the North Portico in 1829. Because of crowding within the executive mansion itself, President Theodore Roosevelt had all work offices relocated to the newly constructed West Wing in 1901. Eight years later, in 1909, President William Howard Taft expanded the West Wing and created the first Oval Office, which was eventually moved and expanded. In the Executive Residence, the third floor attic was converted to living quarters in 1927 by augmenting the existing hip roof with long shed dormers. A newly constructed East Wing was used as a reception area for social events; Jefferson's colonnades connected the new wings. The East Wing alterations were completed in 1946, creating additional office space. By 1948, the residence's load-bearing walls and wood beams were found to be close to failure. Under Harry S. Truman, the interior rooms were completely dismantled and a new intern ------------------------------ Date: Sat, 20 Apr 2024 09:50:50 +0200 From: "Sexual Function" Subject: Eating this for breakfast saves your prostate? (60 seconds) Eating this for breakfast saves your prostate? (60 seconds) http://cooleases.za.com/_nOCYZcZFM-cU-rdK2bhnnBTH-zBsiG5NT0CjbTvRJZpHJa6MQ http://cooleases.za.com/TMJFNZumU1JA70mqWRei5RFUhjTl1mpVsUJQmriMBh8Q7H6yQg ailways were a formalised development of industrial tramways, which had found need on occasions to add additional braking capacity by adding an empty truck to the rear of a group of tramcars. This allowed the "locomotive" b often a cableway powered by a steam engine at the surface b to operate both safely and, more importantly, at higher speed. The first railways, such as the pioneering Liverpool and Manchester Railway of 1830, used a version of the tramways buffer and chain coupling, termed a screw-coupling. Vehicles are coupled by hand using a hook and links with a turnbuckle-like device that draws the vehicles together. Vehicles have buffers, one at each corner on the ends, which are pulled together and compressed by the coupling device. With no continuous brake across the entire train, the whole train was reliant on the braking capacity of the locomotive, and train lengths were restricted. To allow for longer trains, early railway companies from the 1840s onwards began replicating industrial tramway practises, by adding "break vans". The term was derived from their name on the industrial tramways, in which they controlled the (residual) train if there was a "break" in the linkage to the locomotive.[citation needed] Early railway couplings had been found to be prone to breakages. The term was only replaced by "brake van" from the 1870s onwards. Because of the combined risks of shortage of brake power and breaking couplings, the speed of freight trains was initially restricted to 25 mph (40 km/h). The brake van was marshalled at the rear of the train, and served two purposes: Provided additional braking for 'unfitted' goods trains Put a man (the guard) at the rear of the train, who could take action in the event of a breakdown or accident While the UK railway system persisted until post-nationalisation in 1948 with "unfitted" (discontinuously braked) trains and loose couplings (the final unfitted trains ran in the 1990s), other systems, such as the North American adoption of the Janney coupler, overcame the same railway safety issues in a different manner. The guard's duties This section does not cite any sources. Please help improve this section by adding citations to reliable sources. Unsourced material may be challenged and removed. (January 2015) (Learn how and when to remove this template message) On unfitted trains, the brake van has several purposes, and hence jobs for the guard: Operating the brake, train supervision, and illumination & communication. Firstly, and most importantly, the guard would use the brake van's brakes to a ------------------------------ Date: Sat, 20 Apr 2024 11:52:13 +0200 From: "Sexual Health Consultant" Subject: Revitalize Your Relationship with E.D. Elixir Revitalize Your Relationship with E.D. Elixir http://setyardtuiops.za.com/KbYGCh6iSFFlsfbk1SQhaM6FILcsW9TWfPRj6r03-wq1qj4Qpw http://setyardtuiops.za.com/im5C8Aye25sCOvJq4K2MEkwgFfG5enD0PfZJxUXMK-UePThEmA ndesite is an aphanitic (fine-grained) to porphyritic (coarse-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the feldspar in the rock consisting of plagioclase. This places andesite in the basalt/andesite field of the QAPF diagram. Andesite is further distinguished from basalt by its silica content of over 52%. However, it is often not possible to determine the mineral composition of volcanic rocks, due to their very fine grain size, and andesite is then defined chemically as volcanic rock with a content of 57% to 63% silica and not more than about 6% alkali metal oxides. This places the andesite in the O2 field of the TAS classification. Basaltic andesite, with a content of 52% to 57% silica, is represented by the O1 field of the TAS classification but is not a distinct rock type in the QAPF classification. Andesite is the extrusive equivalent of diorite. Andesite is usually light to dark grey in colour, due to its content of hornblende or pyroxene minerals. but can exhibit a wide range of shading. Darker andesite can be challenging to distinguish from basalt, but a common rule of thumb, used away from the laboratory, is that andesite has a color index less than 35. The plagioclase in andesite varies widely in sodium content, from anorthite to oligoclase, but is typically andesine, in which anorthite makes up about 40 mol% of the plagioclase. The pyroxene minerals that may be present include augite, pigeonite, or orthopyroxene. Magnetite, zircon, apatite, ilmenite, biotite, and garnet are common accessory minerals. Alkali feldspar may be present in minor amounts. Andesite is usually porphyritic, containing larger crystals (phenocrysts) of plagioclase formed prior to the extrusion that brought the magma to the surface, embedded in a finer-grained matrix. Phenocrysts of pyroxene or hornblende are also common. These minerals have the highest melting temperatures of the typical minerals that can crystallize from the melt and are therefore the first to form solid crystals. Classification of andesites may be refined according to the ------------------------------ Date: Sat, 20 Apr 2024 10:07:31 +0200 From: "Online Surveys" Subject: Your Experience with State Farm Your Experience with State Farm http://wifirouter.za.com/hqRF6gH_hiPp9UQF1ohz0OefrH170xnkydFuNMQHrMo1fYdi http://wifirouter.za.com/2wPImpr4wMzVY3SN1qvBPb8FXGW3Xu72fUxHgKFU4CjnMxFmuQ ndesite is an aphanitic (fine-grained) to porphyritic (coarse-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the feldspar in the rock consisting of plagioclase. This places andesite in the basalt/andesite field of the QAPF diagram. Andesite is further distinguished from basalt by its silica content of over 52%. However, it is often not possible to determine the mineral composition of volcanic rocks, due to their very fine grain size, and andesite is then defined chemically as volcanic rock with a content of 57% to 63% silica and not more than about 6% alkali metal oxides. This places the andesite in the O2 field of the TAS classification. Basaltic andesite, with a content of 52% to 57% silica, is represented by the O1 field of the TAS classification but is not a distinct rock type in the QAPF classification. Andesite is the extrusive equivalent of diorite. Andesite is usually light to dark grey in colour, due to its content of hornblende or pyroxene minerals. but can exhibit a wide range of shading. Darker andesite can be challenging to distinguish from basalt, but a common rule of thumb, used away from the laboratory, is that andesite has a color index less than 35. The plagioclase in andesite varies widely in sodium content, from anorthite to oligoclase, but is typically andesine, in which anorthite makes up about 40 mol% of the plagioclase. The pyroxene minerals that may be present include augite, pigeonite, or orthopyroxene. Magnetite, zircon, apatite, ilmenite, biotite, and garnet are common accessory minerals. Alkali feldspar may be present in minor amounts. Andesite is usually porphyritic, containing larger crystals (phenocrysts) of plagioclase formed prior to the extrusion that brought the magma to the surface, embedded in a finer-grained matrix. Phenocrysts of pyroxene or hornblende are also common. These minerals have the highest melting temperatures of the typical minerals that can crystallize from the melt and are therefore the first to form solid crystals. Classification of andesites may be refined according to the ------------------------------ Date: Sat, 20 Apr 2024 12:03:20 +0200 From: "Exciting Vacay with Vacabee" Subject: Let's Plan Your Dream Escape with Vacabee! Let's Plan Your Dream Escape with Vacabee! http://promindcomplexzz.za.com/LxbxYJDXwGANWneEUDab5F6zmDkASKdZjQdM8KNTL1TINkMJ http://promindcomplexzz.za.com/AgUYzyMt6mclwz_J4hwuYTIqrZIIwDWtfBB9oYoyO8NjKOwH hless beaked jaws, the laying of hard-shelled eggs, a high metabolic rate, a four-chambered heart, and a strong yet lightweight skeleton. Birds live worldwide and range in size from the 5.5 cm (2.2 in) bee hummingbird to the 2.8 m (9 ft 2 in) common ostrich. There are over 11,000 living species, more than half of which are passerine, or "perching" birds. Birds have wings whose development varies according to species; the only known groups without wings are the extinct moa and elephant birds. Wings, which are modified forelimbs, gave birds the ability to fly, although further evolution has led to the loss of flight in some birds, including ratites, penguins, and diverse endemic island species. The digestive and respiratory systems of birds are also uniquely adapted for flight. Some bird species of aquatic environments, particularly seabirds and some waterbirds, have further evolved for swimming. The study of birds is called ornithology. Birds are feathered theropod dinosaurs and constitute the only known living dinosaurs. Likewise, birds are considered reptiles in the modern cladistic sense of the term, and their closest living relatives are the crocodilians. Birds are descendants of the primitive avialans (whose members include Archaeopteryx) which first appeared during the Late Jurassic. According to recent estimates, modern birds (Neornithes) evolved in the Late Cretaceous and diversified dramatically around the time of the CretaceousbPaleogene extinction event 66 million years ago, which killed off the pterosaurs and all non-avian dinosaurs. Many social species pass on knowledge across generations, which is considered a form of culture. Birds are social, communicating with visual signals, calls, and songs, and participating in such behaviours as cooperative breeding and hunting, flocking, and mobbing of predators. The vast majority of bird species are socially (but not necessarily sexually) monogamous, usually for one breeding season at a time, sometim ------------------------------ End of alt.music.moxy-fruvous digest V14 #13753 ***********************************************