From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #4719 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, August 8 2020 Volume 14 : Number 4719 Today's Subjects: ----------------- How To Build Your Own SHTF Silencer At Home (100% legal) ["Christopher" <] Get good night's sleep ["Daily Health" ] ---------------------------------------------------------------------- Date: Sat, 8 Aug 2020 04:53:43 -0400 From: "Christopher" Subject: How To Build Your Own SHTF Silencer At Home (100% legal) How To Build Your Own SHTF Silencer At Home (100% legal) http://ketoafterr.buzz/x9qM9LfFfHV8TV5RrxP2PfGHIvl9WKTzInLT5N5Xv_66kZf9 http://ketoafterr.buzz/sXWFrPg7MMakL34jkXVhyC0xu3U4vEIRrlAUKI8G79FOUq9n In the United States Army, sappers are combat engineers who support the front-line infantry, and they have fought in every war in U.S. history. For example, after the Battle of Yorktown, General Washington cited Louis LebC(gue Duportail, the chief of engineers, for conduct that afforded "brilliant proofs of his military genius." Modern-day designation as a sapper is earned as an additional proficiency. The U.S. Army authorizes four skill tabs for permanent wear above the unit patch on the left shoulder (Army Regulation 670-1 Chapter 29b13, Sub-Paragraph f). Along with the Sapper Tab, the Special Forces Tab, Ranger Tab, and President's Hundred Tab identify soldiers who have passed a demanding course of military instruction and have demonstrated their competence in particular specialties and skills. To wear the Sapper Tab, a soldier must graduate from the Sapper Leader Course, which is operated by the U.S. Army Engineer School at Fort Leonard Wood, Missouri. The Sapper Leader Course is a demanding 28-day leadership development course for combat engineers that reinforces critical skills and teaches advanced techniques needed across the army. This course is also designed to build esprit de corps by training soldiers in troop-leading procedures, demolitions (conventional and expedient), and mountaineering operations. The course culminates in an intense field-training exercise that reinforces the use of the battle drills and specialized engineering techniques learned throughout the course. The course is open to enlisted soldiers in the grades of E-4 (P) (in the army, specialists on the list for promotion to sergeant) through E-7, cadets, and officers O-2 (first lieutenant ) and below. The course is primarily for U.S. Army and USMC combat engineers, but may be attended by all service members with an approved waiver. PAVN and Viet Cong Sapper formation- PAVN/Viet Cong PAVN (People's Army of Vietnam) and Viet Cong sappers, as they were called by US forces, are better described as commando units. The Vietnamese term ??c cC4ng can be literally translated as "special task". Thousands of specially trained elite fighters served in the PAVN and Viet Cong commandobsapper units which were organized as independent formations. While not always successful due to lack of appropriate personal weapon types for combat and assault like other special forces, at times they inflicted heavy damage against their enemies. They have been armed with various types of bombs, mines, explosive charges, grenades and even steel-pellet mines which were much more devastating than the U.S. M18 Claymore[citation needed] and are still the main weapons of the ??c cC4ng. These elite units served as raiders against American/ARVN troops, and infiltrated spearheads during the final Ho Chi Minh Campaign in 1975, where they seized key road and bridge assets, destroyed installations, attacked command and control nodes located deep inside enemy territory, planted explosives on U.S. water craft, and otherwise helped the PAVN's rapid mobile forces advance. A typical PAVN/VC ??c cC4ng organization is shown in the diagram. The raiding force was usually grouped into assault teams, each broken down into several 3b5 man assault cells. Overall, there were generally four operational echelons. An instance of a successful sapper attack conducted by the Viet Cong was the during the Battle of Fire Base Mary Ann. A small number of sappers, through surprise, conducted a successful attack on a superior US force. The battle was described as a "rampage of VC who threw satchels at the command bunker, knifed Americans in their sleep and destroyed all communications equipmen ------------------------------ Date: Sat, 8 Aug 2020 07:04:20 -0400 From: "Daily Health" Subject: Get good night's sleep Get good night's sleep http://battles.click/DZ2fFneKOJL7vQWzrKBJBFUpB0iHJeOfPvPjiLb8OxANnOQg http://battles.click/WSaIJSwLg6dy05upKRdfp5yt-56VOYGT63C4WPfMaeJmFwd9 The amount of oxygen found in seawater depends primarily on the plants growing in it. These are mainly algae, including phytoplankton, with some vascular plants such as seagrasses. In daylight the photosynthetic activity of these plants produces oxygen, which dissolves in the seawater and is used by marine animals. At night, photosynthesis stops, and the amount of dissolved oxygen declines. In the deep sea, where insufficient light penetrates for plants to grow, there is very little dissolved oxygen. In its absence, organic material is broken down by anaerobic bacteria producing hydrogen sulphide. Global warming is likely to reduce levels of oxygen in surface waters, since the solubility of oxygen in water falls at higher temperatures. The amount of light that penetrates the sea depends on the angle of the sun, the weather conditions and the turbidity of the water. Much light gets reflected at the surface, and red light gets absorbed in the top few metres. Yellow and green light reach greater depths, and blue and violet light may penetrate as deep as 1,000 metres (3,300 ft). There is insufficient light for photosynthesis and plant growth beyond a depth of about 200 metres (660 ft). Waves File:Steep deep water wave.ogv Movement of molecules as waves pass Diagram showing wave approaching shore When the wave enters shallow water, it slows down and its amplitude (height) increases. Main article: Wind wave Wind blowing over the surface of a body of water forms waves that are perpendicular to the direction of the wind. The friction between air and water caused by a gentle breeze on a pond causes ripples to form. A strong blow over the ocean causes larger waves as the moving air pushes against the raised ridges of water. The waves reach their maximum height when the rate at which they are travelling nearly matches the speed of the wind. In open water, when the wind blows continuously as happens in the Southern Hemisphere in the Roaring Forties, long, organised masses of water called swell roll across the ocean.(pp83b84) If the wind dies down, the wave formation is reduced, but already-formed waves continue to travel in their original direction until they meet land. The size of the waves depends on the fetch, the distance that the wind has blown over the water and the strength and duration of that wind. When waves meet others coming from different directions, interference between the two can produce broken, irregular seas. Constructive interference can cause individual (unexpected) rogue waves much higher than normal. Most waves are less than 3 m (10 ft) high and it is not unusual for strong storms to double or triple that height; offshore construction such as wind farms and oil platforms use metocean statistics from measurements in computing the wave forces (due to for instance the hundred-year wave) they are designed against. Rogue waves, however, have been documented at heights above 25 meters (82 ft). The top of a wave is known as the crest, the lowest point between waves is the trough and the distance between the crests is the wavelength. The wave is pushed across the surface of the sea by the wind, but this represents a transfer of energy and not a horizontal movement of water. As waves approach land and move into shallow water, they change their behavior. If approaching at an angle, waves may bend (refraction) or wrap rocks and headlands (diffraction). When the wave reaches a point where its deepest oscillations of the water contact the seabed, they begin to slow down. This pulls the crests closer together and increases the waves' height, which is called wave shoaling. When the ratio of the wave's height to the water depth increases above a certain limit, it "breaks", toppling over in a mass of foaming water. This rushes in a sheet up the beach before retreating into the sea under the influence of grav ------------------------------ End of alt.music.moxy-fruvous digest V14 #4719 **********************************************