From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #4037 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, April 24 2020 Volume 14 : Number 4037 Today's Subjects: ----------------- Have You Given Asian Dating a Try? ["Asian Beauty" Subject: Have You Given Asian Dating a Try? Have You Given Asian Dating a Try? http://ultramoskihack.buzz/3HLiqGqxbsWt32_Vl0o3IWJNNP6Cai4HD_f5j7DfasbFgi8 http://ultramoskihack.buzz/qkOkKdeMcswrDrRi1iYUavDAbXtJIHVZrIT5mdBqmoJBOus as the Sandwich Islands. With Hiram Clark presiding, the missionaries included Elders Henry Bigler, Hiram Blackwell, George Q. Cannon, John Dixon, William Farrer, James Hawkins, James Keeler, Thomas Morris, and Thomas Whittle. A day after their arrival the group climbed a hill above Honolulu (Pacific Heights), constructed a small, makeshift altar and said a prayer. A week later, the ten missionaries received their assignments: Farrer and Dixon headed to the island of Kaua'i, Cannon, Keeler, and Bigler to Lahaina on the island of Maui, Blackwell and Hawkins to the Big Island of Hawaii, with Morris, Whittle, and Clark staying behind in Honolulu. This group formed the basis of the Sandwich Islands Mission. The first church congregation in Hawaii was established on the island of Maui in 1851. Among the early converts of Cannon were three prominent native Hawaiians: Napela, Uaua and Kaleohano who would later serve as prominent missionaries and leaders in the LDS Church. Missionaries lead a group of Hawaiian Latter-day Saints in establishing a colony on the island of L?na?i in 1854. In 1857 the American missionaries left due to the Utah War. No new missionaries came until Walter Murray Gibson arrived in 1861. Gibson instituted irregular activities such as selling the priesthood. Some local leaders, such as Napela, sent letters to Salt Lake City asking for Gibson to be replaced. In response, Ezra T. Benson and Lorenzo Snow of the church's Quorum of the Twelve Apostles were sent to take over the leadership of the mission, with the assistance of Joseph F. Smith, who had been a missionary in Hawaii for much of the 1850s. Most of the membership followed Benson, Snow, and Smith, but in the process ownership of the property on Lanai was lost. A new colony for Hawaiian Latter-day Saints was established ------------------------------ Date: Fri, 24 Apr 2020 06:57:42 -0400 From: "Kill Insects" Subject: Keep on reading to claim your special 50% off offer below... Keep on reading to claim your special 50% off offer below... http://moskidiy.live/YsxtRxhCxhK22d_wTTO_Fa18ATrtUc-y4aMBePOwO0wRSbB9 http://moskidiy.live/qArSNlwW0oHNTKr_eKmhMOHz-sdNPvU1bR1CMvxdA9lX9Hk rock layers above. Much of the lower continental crust is metamorphic, except for recent igneous intrusions. Horizontal tectonic movements such as the collision of continents create orogenic belts, and cause high temperatures, pressures and deformation in the rocks along these belts. If the metamorphosed rocks are later uplifted and exposed by erosion, they may occur in long belts or other large areas at the surface. The process of metamorphism may have destroyed the original features that could have revealed the rock's previous history. Recrystallization of the rock will destroy the textures and fossils present in sedimentary rocks. Metasomatism will change the original composition. Regional metamorphism tends to make the rock more indurated and at the same time to give it a foliated, shistose or gneissic texture, consisting of a planar arrangement of the minerals, so that platy or prismatic minerals like mica and hornblende have their longest axes arranged parallel to one another. For that reason many of these rocks split readily in one direction along mica-bearing zones (schists). In gneisses, minerals also tend to be segregated into bands; thus there are seams of quartz and of mica in a mica schist, very thin, but consisting essentially of one mineral. Along the mineral layers composed of soft or fissile minerals the rocks will split most readily, and the freshly split specimens will appear to be faced or coated with this mineral; for example, a piece of mica schist looked at facewise might be supposed to consist entirely of shining scales of mica. On the edge of the specimens, however, the white folia of granular quartz will be visible. In gneisses these alternating folia are sometimes thicker and less regular than in schists, but most importantly less micaceous; they may be lenticular, dying out rapidly. Gneisses also, as a rule, contain more feldspar than schists do, and are tougher and less fissile. Contortion or crumbling of the foliation is by no means uncommon; splitting faces are undulose or puckered. Schistosity and gneissic banding (the two main types of foliation) are formed by directed pressure at elevated temperature, and to interstitial movement, or internal flow arranging the mineral particles while they are crystallizing in that directed pressure field. ------------------------------ Date: Fri, 24 Apr 2020 05:49:37 -0400 From: "HD TV" Subject: Super Smartwave Anntenna is easy to use Super Smartwave Anntenna is easy to use http://ultramoskihack.buzz/MX7FWSn568niAUJ-iKPLt88voC7AYJ7ZN2tBEb4cKYcxKA http://ultramoskihack.buzz/Wq2Dt0P7FGumxtV4kxtI8ZtKb8afg_AcRYgThdnnmhq7bA parks and monuments are sometimes referred to metaphorically as "crown jewels". The system encompasses approximately 84.4 million acres (338,000 kmB2), of which more than 4.3 million acres (17,000 kmB2) remain in private ownership. The largest unit is WrangellbSt. Elias National Park and Preserve, Alaska. At 13,200,000 acres (53,000 kmB2), it is over 16 percent of the entire system. The smallest unit in the system is Thaddeus Kosciuszko National Memorial, Pennsylvania, at 0.02 acre (80 mB2). In addition to administering its units and other properties, the National Park Service also provides technical and financial assistance to several "affiliated areas" authorized by Congress. The largest affiliated area is New Jersey Pinelands National Reserve at 1,164,025 acres (4711 kmB2). The smallest is Benjamin Franklin National Memorial at less than 0.01 acres (40 m2). Although all units of the National Park System in the United States are the responsibility of a single agency, they are all managed under individual pieces of authorizing legislation or, in the case of national monuments created under the Antiquities Act, presidential proclamation. For example, because of provisions within their enabling legislation, Congaree National Park is almost entirely wilderness area devoid of development, yet Yosemite allows unique developments such as the Badger Pass Ski Area and the O'Shaughnessy Dam within its boundaries. Death Valley National Park has an active mine legislated within its boundaries. Such irregularities would not be found in other parks unless specifically provided for with exceptions by the legislation that created them ------------------------------ Date: Thu, 23 Apr 2020 13:44:19 -0400 From: "**5 Myths of CBD**" <**5MythsofCBD**@cbdonly.guru> Subject: More Effective Than Aspirin?! More Effective Than Aspirin?! http://cbdonly.guru/XHo4M7PQMwmEYYsSE9dfi6HPmqH7i0w9p95vL_4S2c9y-3Q http://cbdonly.guru/Tjg8__71s8AAemFflJFKo-vHcqIRMt55cGs6794RtSYfSGo Early Medieval architecture's secular buildings were simple constructions mainly using timber with thatch for roofing. Ecclesiastical architecture ranged from a synthesis of HibernobSaxon monasticism, to Early Christian basilica and architecture characterised by pilaster-strips, blank arcading, baluster shafts and triangular headed openings. After the Norman conquest in 1066 various Castles in England were created so law lords could uphold their authority and in the north to protect from invasion. Some of the best-known medieval castles are the Tower of London, Warwick Castle, Durham Castle and Windsor Castle. A castle of square plan surrounded by a water-filled moat. It has round corner towers and a forbidding appearance. Bodiam Castle is a 14th-century moated castle near Robertsbridge in East Sussex. Throughout the Plantagenet era, an English Gothic architecture flourished, with prime examples including the medieval cathedrals such as Canterbury Cathedral, Westminster Abbey and York Minster. Expanding on the Norman base there was also castles, palaces, great houses, universities and parish churches. Medieval architecture was completed with the 16th-century Tudor style; the four-centred arch, now known as the Tudor arch, was a defining feature as were wattle and daub houses domestically. In the aftermath of the Renaissance a form of architecture echoing classical antiquity synthesised with Christianity appeared, the English Baroque style of architect Christopher Wren being particularly championed. Georgian architecture followed in a more refined style, evoking a simple Palladian form; the Royal Crescent at Bath is one of the best examples of this. With the emergence of romanticism during Victorian period, a Gothic Revival was launched. In addition to this, around ------------------------------ Date: Fri, 24 Apr 2020 04:45:36 -0400 From: "Christopher" Subject: How To Build Your Own Military-Grade Silencer At Home (100% legal) How To Build Your Own Military-Grade Silencer At Home (100% legal) http://ultramoskihack.buzz/cIGXd2um9qqfnDQWpz6pGnEv8MGSFe1-ZDdyGYLehM327rQ http://ultramoskihack.buzz/LlWTXt5GC4E_AB1QEOgvZOj_WFnozJtlMKmlXWBAJrf_4JM Money supply data is recorded and published, usually by the government or the central bank of the country. Public and private sector analysts monitor changes in the money supply because of the belief that such changes affect the price level of securities, inflation, the exchange rates and the business cycle. The relationship between money and prices has historically been associated with the quantity theory of money. There is strong empirical evidence of a direct relationship between the growth of the money supply and long-term price inflation, at least for rapid increases in the amount of money in the economy. For example, a country such as Zimbabwe which saw extremely rapid increases in its money supply also saw extremely rapid increases in prices (hyperinflation). This is one reason for the reliance on monetary policy as a means of controlling inflation. The nature of this causal chain is the subject of some debate. Some heterodox economists argue that the money supply is endogenous (determined by the workings of the economy, not by the central bank) and that the sources of inflation must be found in the distributional structure of the economy. In addition, those economists seeing the central bank's control over the money supply as feeble say that there are two weak links between the growth of the money supply and the inflation rate. First, in the aftermath of a recession, when many resources are underutilized, an increase in the money supply can cause a sustained increase in real production instead of inflation. Second, if the velocity of money (i.e., the ratio between nominal GDP and money supply) changes ------------------------------ Date: Thu, 23 Apr 2020 18:51:04 +0200 From: " wireless-N mini extender" Subject: A powerful Wi-Fi in every single inch of your home! This email must be viewed in HTML mode. ------------------------------ Date: Fri, 24 Apr 2020 05:22:00 -0400 From: "MeetRussianLady" Subject: If You Want Her, Come And Get Her If You Want Her, Come And Get Her http://boostfit.buzz/J7zlYjtJBxX3o0dvuQt-fTNye9EoZfdk2qjnwzpFYd3g4Ro http://boostfit.buzz/SSyMQJgupL-DTAsXU2pN8UAv5kkYUWOJSkbFz-nDnQDrs6-z agencies, including the California Department of Transportation (Caltrans), San Francisco Municipal Transportation Agency, and the Metropolitan Transportation Commission. These and other organizations collectively manage several interstate highways and state routes, two subway networks, two commuter rail agencies, eight trans-bay bridges, transbay ferry service, local bus service, three international airports (San Francisco, San Jose, and Oakland), and an extensive network of roads, tunnels, and paths such as the San Francisco Bay Trail. The Bay Area hosts an extensive freeway and highway system that is particularly prone to traffic congestion, with one study by Inrix concluding that the Bay Area's traffic was the fourth worst in the world. There are some city streets in San Francisco where gaps occur in the freeway system, partly the result of the Freeway Revolt, which prevented a freeway-only thoroughfare through San Francisco between the San FranciscobOakland Bay Bridge, the western terminus of Interstate 80, and the southern terminus of the Golden Gate Bridge (U.S. Route 101). Additional damage that occurred in the wake of the 1989 Loma Prieta earthquake resulted in freeway segments being removed instead of being reinforced or rebuilt, leading to the revitalization of neighborhoods such as San Francisco's Embarcadero and Hayes Valley. The greater Bay Area contains the three principal northbsouth highways in California: Interstate 5, U.S. Route 101, and California State Route 1. U.S. 101 and State Route 1 directly serve the traditional nine-county region, while Interstate 5 bypasses to the east in San Joaquin County to provide a more direct Los AngelesbSacramento route. Additional local highways connect the various subregions of the Bay Area together ------------------------------ Date: Fri, 24 Apr 2020 07:14:33 -0400 From: "Teach Your child" Subject: Reading Makes Your Child Smarter Reading Makes Your Child Smarter http://moneydial.bid/t8kZmUgzgYTMgAXbMruHd9LQhtqVZzi70MbYjoJuG9vkfKoy http://moneydial.bid/nDAJOaTe3Zr2P71u1H8NOaOSgQcwTG5mu05F2bgk9xoe_Oc Around the igneous rock that forms from the cooling magma is a metamorphosed zone called a contact metamorphism aureole. Aureoles may show all degrees of metamorphism from the contact area to unmetamorphosed (unchanged) country rock some distance away. The formation of important ore minerals may occur by the process of metasomatism at or near the contact zone. When a rock is contact altered by an igneous intrusion it very frequently becomes more indurated, and more coarsely crystalline. Many altered rocks of this type were formerly called hornstones, and the term hornfels is often used by geologists to signify those fine grained, compact, non-foliated products of contact metamorphism. A shale may become a dark argillaceous hornfels, full of tiny plates of brownish biotite; a marl or impure limestone may change to a grey, yellow or greenish lime-silicate-hornfels or siliceous marble, tough and splintery, with abundant augite, garnet, wollastonite and other minerals in which calcite is an important component. A diabase or andesite may become a diabase hornfels or andesite hornfels with development of new hornblende and biotite and a partial recrystallization of the original feldspar. Chert or flint may become a finely crystalline quartz rock; sandstones lose their clastic structure and are converted into a mosaic of small close-fitting grains of quartz in a metamorphic rock called quartzite. If the rock was originally banded or foliated (as, for example, a laminated sandstone or a foliated calc-schist) this character may not be obliterated, and a banded hornfels is the product; fossils even may have their shapes preserved, though entirely recrystallized, and in many contact-altered lavas the vesicles are still visible, though their contents have usually entered into new combinations to form minerals that were not originally present. The minute structures, however, disappear, often completely, if the thermal alteration is very profound. Thus small grains of quartz in a shale are lost or blend with the surrounding particles of clay, and the fine ground-mass of lavas is entirely reconstructed ------------------------------ End of alt.music.moxy-fruvous digest V14 #4037 **********************************************