From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #11048 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 Sunday, April 2 2023 Volume 14 : Number 11048 Today's Subjects: ----------------- Reverse blurriness in 10 minutes with this? ["Vision loss" Subject: Reverse blurriness in 10 minutes with this? Reverse blurriness in 10 minutes with this? http://whowhoplatinumz.shop/IqzSM-oowxsGxoutfuKXkFFrtPgbaCWDRb4DFSw2pT-mD-FDkQ http://whowhoplatinumz.shop/4gVdI3YfzKv9qN9FOyvn0Q_6dHQ43hJ6D3BFTJ5w94L7aiUM8A it has a volume of 50 millionUS gallons (190 million L). With the new reservoir came improvements to the Powell Butte park, including resurfaced and realigned trails, reduced environmental impacts, better accessibility measures, and reduction of steep grades. The government also built a visitor center, caretaker's house, public restrooms, maintenance yard, and a permeable parking area that permitted filtration of rainwater through asphalt to an underground stone bed, where it could be absorbed by the soil and then into the nearest aquifer. Built between 1993 and 1998, the Robertson Tunnel runs for 3 miles (4.8 km) through the Tualatin Mountains. It contains Washington Park station, the deepest train station in North America, located 260 feet (80 m) underground. The station displays a core that exhibits Boring Lava deposits. For the first 3,900 feet (1,200 m) of the tunnel, the core shows Boring lava flows with cinder, breccia, and loess dated from 1.47 million to 120,000 years ago, which have been deformed by the Sylvan fault. With the Oatfield fault, the Sylvan fault trends to the northwest, extending 9.3 miles (15 km) northwest and 16 miles (25 km) southeast of the tunnel. It is of Quaternary age and lacks surface expression, possibly as a result of its extensive burial by loess along its length. In 2000, the nonprofit Friends of Mt. Tabor Park was formed to help maintain the Mount Tabor Park area, located 3.5 miles (5.6 km) east of downtown Portland. They have an organizational website and publish a bi-annual newsletter called the Tabor Times. Membership requires dues, and they also rely on donations and a gift shop for financial support. In September 2017, the Hogan Butte Nature Park opened in the city of Gresham, encompassing an area of 46 acres (19 ha) that includes the extinct Boring Lava Field volcano Hogan Butte. This park opened after more than 25 years of processing, supported by a 1990 bond from the city and two regional Metro bonds. Collaborators for opening the park include the U.S. Forest Service, local citizens, Metro, The Trust for Public Land, and the Buttes Conservancy organization. Gresham is one of just a few places in the United States with volcanoes contained in its city limits. Mount Sylvania and Mount Scott lie within the limits of Portland, in the southwestern and southeastern parts of the city, respec ------------------------------ Date: Sat, 1 Apr 2023 16:35:49 +0200 From: "Larger & Stronger" Subject: Scientifically proven remedy for Thick & Rock-Hard Erections Scientifically proven remedy for Thick & Rock-Hard Erections http://bactolife.today/RBW4MsZVduc1YbpLdasrEJyg-CVN7qxKO6lM7Lf1OFDuED4R4w http://bactolife.today/gRjueCpSX7DL6tjLqQESZNhwpIPimxwTrgh7BUX0VqlNlcwHOw altic andesite predominate among Boring Lava deposits. The olivine basalt deposits have fine to medium textures, and the basaltic andesite lava flow deposits have relatively little pyroclastic rock in them, suggesting that explosive eruptions were uncommon within the field. Dark gray to light gray in color, Boring Lava produces columnar and platy joints, which can be seen in Oregon east of Portland and in Clark County in Washington state. It is usually phyric, though one sample from Rocky Butte consists of labradorite with olivine phenocrysts that have been transformed to iddingsite. The Boring Lava reaches thicknesses of more than 400 feet (120 m). Boring Lava has a more mafic (rich in magnesium in iron) composition than the nearby volcano Mount Hood, but they are similar in age. There is a small amount of andesite in the lavas from the field, mostly erupted from monogenetic vents or Larch Mountain. Sometimes, Boring Lava overlaps with volcaniclastic conglomerate from other Cascade eruptions in Multnomah County and the northern part of Clackamas County. The Boring Lava also contains tuff, cinder, and scoria; it is characterized by plagioclase laths that show a pilotaxitic texture with spaces between them that show a diktytaxitic texture. The Boring Lava exposures show aeromagnetic anomalies with short wavelengths and high amplitudes suggestive of their relatively young geological ages. At points where the Boring Lava sits over Troutdale Formation deposits, landslides are frequent, producing steep head scarps with heights of up to 66 feet (20 m). These scarps tend to have grabens at their bases and Boring Lava blocks at their tops, and they show variable slide surfaces from hummocky to flat. A number of these exposures show dips up to 35 degrees, as well as minor faults. The landslides range in thickness from 20 to 79 feet (6 to 24 m). Portland's wet climate leads to weathering, which at the Boring Lava Field has reached depths of up to 25 feet (7.6 m), altering the upper 5 to 15 feet (1.5 to 4.6 m) of soil to a red, clay-like material. At the cinder cone in Mount Tabor Park, an outcrop of quartzite-pebble xenoliths (rock fragments enveloped in a larger rock during the latter's development and solidification) can be observed among local cinder specimens, dating from Miocene to Pliocene Troutdale deposits. While the volcanic rock of Boring Lava was being emplaced over rock from the Troutdale formation, there was deformation that uplifted and dropped fault blocks to the southeast of Portland. Along the Washougal River, a large landslide occurred as a result of failure due to the Boring Lava pushing down on rock from the Troutdale formation. Intrusions of Boring Lava formed outcrops at Highland Butte, La Butte, and potentially in the subsurface regions near Aurora and Curtis, and these intrusions have ------------------------------ Date: Sat, 1 Apr 2023 13:58:39 +0200 From: "Loweâs Order Update" Subject: Your Participation is Needed! Your Participation is Needed! http://clarisils.today/8ZkcFnN8zliZiStiPOTpoJAHQ1REFHj9pvQ8xsyxP_pMrUW2_A http://clarisils.today/Rt1IEsgx0cpfjKOBDRExWCTE200KkaXj_E04ZODfOsLbd7pAnA The Boring Lava Field (also known as the Boring Volcanic Field) is a Plio-Pleistocene volcanic field with cinder cones, small shield volcanoes, and lava flows in the northern Willamette Valley of the U.S. state of Oregon and adjacent southwest Washington state. The field got its name from the town of Boring, Oregon, located 12 miles (19 km) southeast of downtown Portland. Boring lies southeast of the most dense cluster of lava vents. The zone became volcanically active about 2.7 million years ago, with long periods of eruptive activity interspersed with quiescence. Its last eruptions took place about 57,000 years ago at the Beacon Rock cinder cone volcano; the individual volcanic vents of the field are considered extinct, but the field itself is not. The volcanic field covers an area of about 1,500 square miles (3,900 km2), and it has a total volume of 2.4 cubic miles (10 km3). This region sustains diverse flora and fauna within its habitat areas, which are subject to Portland's moderate climate with variable temperatures and mild precipitation. The highest elevation of the field is at Larch Mountain, which reaches a height of 4,055 feet (1,236 m). The Portland metropolitan area, including suburbs, is one of the few places in the continental United States to have extinct volcanoes within a city's limits, and the Boring Lava Field plays an important role in local affairs, including the development of the Robertson Tunnel, recreation, and nature parks. Because of the field's proximity to densely populated areas, eruptive activity would be a threat to human life and property, but the probability for future eruptions affecting the PortlandbVancouver metropolitan area is very low. The field may also influence future earthquakes in the area, as intrusive rock from its historic eruptions may affect ground movement ------------------------------ End of alt.music.moxy-fruvous digest V14 #11048 ***********************************************