From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #11057 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 Tuesday, April 4 2023 Volume 14 : Number 11057 Today's Subjects: ----------------- Don't Miss Your Chance to Win a Craftsman Shot Vacuum - Enter Now! ["Targ] Get McAfee Due to an increase in Malware and Ransomware ["McAfee AntiViru] ---------------------------------------------------------------------- Date: Sat, 1 Apr 2023 14:40:12 +0200 From: "Target Unlocked" Subject: Don't Miss Your Chance to Win a Craftsman Shot Vacuum - Enter Now! Don't Miss Your Chance to Win a Craftsman Shot Vacuum - Enter Now! http://clarisils.today/wXfUvsmIDwpY1MHhUNghkJ8XOPcirAKyCiNz81UXFOs_76ymGQ http://clarisils.today/bU7otbKEV8sls9DDCcj2YH8KQ0hOYNR_yaGYpFSaFWVpAtD4kA With a variable topography, the Portland area ranges from river valley floors to terraces reaching elevations of 400 feet (120 m). The Willamette Valley is marked by hills reaching heights of more than 1,000 feet (300 m), and it is also physically separated from the lower Columbia River valley. The Columbia River flows west from the eastern Portland region, merging with the Willamette near Portland before moving north. Tributaries for the Willamette include the Pudding, Molalla, Tualatin, Abernethy, and Clackamas Rivers; tributaries for the Columbia River include the Washougal and Sandy Rivers. The Columbia River has significantly shaped the geology of the area. Multnomah Creek drains from Larch Mountain, one of the volcanic cones in Boring Lava Field. Local streams near the community of Boring receive seepage from the local aquifer. This unit, part of the greater Troutdale sandstone aquifer, is also made of sandstone and conglomerate and bears water well. It also supplies water to domestic wells in the Mount Norway area. Boring Lava is known to have formed intrusions into local sedimentary rock, and thus it may guide flow of groundwater locally. Portland's climate is moderate, with long growing seasons, moderate rainfail, mild winters, and warm, dry summer seasons. The area has more than 200 frost-free days annually. Temperature can vary widely, reaching a historic maximum of 107 B0F (42 B0C), though the usual July maximum is below 80 B0F (27 B0C), and the average minimum for January is above 32 B0F (0 B0C). Yearly, precipitation averages between 35 to 45 inches (89 to 114 cm) in most river valleys, with a mean of 42.04 inches (106.8 cm) from 1871 through 1952. It shows variability, however, with a historic low of 26.11 inches (66.3 cm) at Portland in 1929 and a maximum of 67.24 inches (170.8 cm) in 1882. More than 75 percent of this precipitation occurs between October and March; July and August mark the driest months with means below 1 inch (2.5 cm), while November, December, and January represent the wettest with averages greater than 6 inches (15 cm). Prevailing winds originate from the south during winter and from the northwest during the summer season, with the exception of prevailing winds at the mouth of the Columbia River Gorge, where winds predominantly move to the east. The southern winds have the highest velocities of the three, only rarely occurring with potentially destructive for ------------------------------ Date: Sat, 1 Apr 2023 11:14:15 +0200 From: "McAfee AntiVirus" Subject: Get McAfee Due to an increase in Malware and Ransomware Get McAfee Due to an increase in Malware and Ransomware http://keragenies.best/r8hF1whqb89FBwNfbokeW_9Gu1XMkvRvVNrMofmC6I6sRdyNwQ http://keragenies.best/JqpXVM0ue-QVGf8HmPp1OYtvcIXMWQlNzfDxxLRxUhmsfhBZBw The Boring Lava deposits received their name based on their proximity to the town of Boring, which lies 12 miles (19 km) southeast of downtown Portland. The term "Boring Lava" is often used to refer to the local deposits erupted by vents in the field. They are located in the western portion of Oregon. The deposits were given this name by R. Treasher in 1942. In 2002, as geochemical and geochronological information on the Boring deposits accumulated, they were designated part of the larger Boring Lava Field. This grouping is somewhat informal and is based on similarities in age and lithology. The Boring Lava deposits lie west of the town of Boring. The Global Volcanism Program lists the volcanic field's highest elevation as 4,055 feet (1,236 m), at Larch Mountain; most vents reach an elevation of 660 to 980 feet (200 to 300 m). Located in the Portland Basin, the field consists of monogenetic volcanic cones that appear as hills throughout the area, reaching heights of 650 feet (200 m) above their surroundings. The collection includes more than 80 small volcanic edifices and lava flows in the PortlandbVancouver metropolitan area, with the possibility of more volcanic deposits buried under sedimentary rock layers. The borders for the Boring Lava Field group are clear, except on the eastern side where distinguishing between Boring deposits and those from the major Cascade arc are less clear; many geologists have arbitrarily placed the eastern border at a longitude of 122 degrees west. In total, the Boring Lava Field covers an area of about 1,500 square miles (4,000 km2), and it has a total volume of 2.4 cubic mile ------------------------------ End of alt.music.moxy-fruvous digest V14 #11057 ***********************************************