From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #6987 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 Wednesday, July 21 2021 Volume 14 : Number 6987 Today's Subjects: ----------------- Get Your Free Ankle Holster For Concealed Carry ["Giving Away" Subject: Get Your Free Ankle Holster For Concealed Carry Get Your Free Ankle Holster For Concealed Carry http://dronecamera.us/fFJf-dEK2lqTq1cKgwyjPBrbiJ_yvFb9EPLqTtEBdx-5XCVg http://dronecamera.us/ApvNKIHlvCF4LDeV6bSq2TbvWTDfDbszgOU5BmmqnpY0Qn7j abiting animals are often categorized as troglobites (cave-limited species), troglophiles (species that can live their entire lives in caves, but also occur in other environments), trogloxenes (species that use caves, but cannot complete their life cycle fully in caves) and accidentals (animals not in one of the previous categories). Some authors use separate terminology for aquatic forms (for example, stygobites, stygophiles, and stygoxenes). Of these animals, the troglobites are perhaps the most unusual organisms. Troglobitic species often show a number of characteristics, termed troglomorphic, associated with their adaptation to subterranean life. These characteristics may include a loss of pigment (often resulting in a pale or white coloration), a loss of eyes (or at least of optical functionality), an elongation of appendages, and an enhancement of other senses (such as the ability to sense vibrations in water). Aquatic troglobites (or stygobites), such as the endangered Alabama cave shrimp, live in bodies of water found in caves and get nutrients from detritus washed into their caves and from the feces of bats and other cave inhabitants. Other aquatic troglobites include cave fish, and cave salamanders such as the olm and the Texas blind salamander. Cave insects such as Oligaphorura (formerly Archaphorura) schoetti are troglophiles, reaching 1.7 millimetres (0.067 in) in length. They have extensive distribution and have been studied fairly widely. Most specimens are female, but a male specimen was collected from St Cuthberts Swallet in 1969. Bats, such as the gray bat and Mexican free-tailed bat, are trogloxenes and are often found in caves; they forage outside of the caves. Some species of cave crickets are classified as trogloxenes, because they roost in caves by day and for ------------------------------ Date: Wed, 21 Jul 2021 03:58:06 -0400 From: "Collapse-Survival" Subject: FOX News Compromised! (URGENT) FOX News Compromised! (URGENT) http://prayermiracle.us/mtCUQHUhzxJrcDx5syXDrOWpIKP_Au58Ppi4FnOzW0nu0Vdm http://prayermiracle.us/YO5BR36z6pQRJFuMZ8Ufo8yYRdFlEgH6lKhB2od6g8knmayB ifies. Hot liquid lava continues to flow under that crust, and if most of it flows out, a hollow tube remains. Such caves can be found in the Canary Islands, Jeju-do, the basaltic plains of Eastern Idaho, and in other places. Kazumura Cave near Hilo, Hawaii is a remarkably long and deep lava tube; it is 65.6 km long (40.8 mi). Lava caves include but are not limited to lava tubes. Other caves formed through volcanic activity include rifts, lava molds, open vertical conduits, inflationary, blisters, among others. Sea or littoral Main article: Sea cave Painted Cave, a large sea cave, Santa Cruz Island, California Sea caves are found along coasts around the world. A special case is littoral caves, which are formed by wave action in zones of weakness in sea cliffs. Often these weaknesses are faults, but they may also be dykes or bedding-plane contacts. Some wave-cut caves are now above sea level because of later uplift. Elsewhere, in places such as Thailand's Phang Nga Bay, solutional caves have been flooded by the sea and are now subject to littoral erosion. Sea caves are generally around 5 to 50 metres (16 to 164 ft) in length, but may exceed 300 metres (980 ft). Corrasional or erosional Salt cave in Mount Sodom, Israel. Corrasional or erosional caves are those that form entirely by erosion by flowing streams carrying rocks and other sediments. These can form in any type of rock, including hard rocks such as granite. Generally there must be some zone of weakness to guide the water, such as a fault or joint. A subtype of the erosional cave is the wind or aeolian cave, carved by wind-born sediments. Many caves formed initially by solutional processes often undergo a subsequent phase of erosional or vadose enlargement where active streams or rivers pa ------------------------------ Date: Wed, 21 Jul 2021 03:18:04 -0400 From: "Sam's Club Opinion Requested" Subject: Leave your feedback and you could WIN! Leave your feedback and you could WIN! http://dronecamera.us/EwUu1eW59bIUo4rvyeGXbKEocyWGrPhwHdHqntdUGOHfsP8G http://dronecamera.us/qAGTEvX_0c1rlBSbh0kAAP6t9cSa4LgPgDw6Kn8Q8IHrbdtp utional caves or karst caves are the most frequently occurring caves. Such caves form in rock that is soluble; most occur in limestone, but they can also form in other rocks including chalk, dolomite, marble, salt, and gypsum. Rock is dissolved by natural acid in groundwater that seeps through bedding planes, faults, joints, and comparable features. Over time cracks enlarge to become caves and cave systems. The largest and most abundant solutional caves are located in limestone. Limestone dissolves under the action of rainwater and groundwater charged with H2CO3 (carbonic acid) and naturally occurring organic acids. The dissolution process produces a distinctive landform known as karst, characterized by sinkholes and underground drainage. Limestone caves are often adorned with calcium carbonate formations produced through slow precipitation. These include flowstones, stalactites, stalagmites, helictites, soda straws and columns. These secondary mineral deposits in caves are called speleothems. The portions of a solutional cave that are below the water table or the local level of the groundwater will be flooded. Lechuguilla Cave in New Mexico and nearby Carlsbad Cavern are now believed to be examples of another type of solutional cave. They were formed by H2S (hydrogen sulfide) gas rising from below, where reservoirs of oil give off sulfurous fumes. This gas mixes with groundwater and forms H2SO4 (sulfuric acid). The acid then dissolves the limestone from below, rather than from above, by acidic water percolating from the surface. Primary Exploring a lava tube in Hawaii. Caves formed at the same time as the surrounding rock are called primary caves. Lava tubes are formed through volcanic activity and are the most common pri ------------------------------ Date: Wed, 21 Jul 2021 11:10:05 +0200 From: "Neck Massager" Subject: NeckMassager : Ultimate Solution To Chronic Neck Pain Content-Transfer-Encoding: 8bit ------------------------------ Date: Wed, 21 Jul 2021 03:05:03 -0400 From: "Bank of America Shopper Gift Card Chance" Subject: Congratulations! You can get a $50 Bank of America gift card! Congratulations! You can get a $50 Bank of America gift card! http://prayermiracle.us/Qp_7C9J-hTF_-de4mfOlIZizPUZ12EGSwO9q1oolkLrOP5GF http://prayermiracle.us/M3OuSqkyGLhxnfZEWn5P2dlp0LDc2Z55lO_tJb84qonkI0lt ation and development of caves is known as speleogenesis; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganisms, pressure, and atmospheric influences. Isotopic dating techniques can be applied to cave sediments, to determine the timescale of the geological events which formed and shaped present-day caves. It is estimated that a cave cannot be more than 3,000 metres (9,800 ft) vertically beneath the surface due to the pressure of overlying rocks. This does not, however, impose a maximum depth for a cave which is measured from its highest entrance to its lowest point, as the amount of rock above the lowest point is dependent on the topography of the landscape above it. For karst caves the maximum depth is determined on the basis of the lower limit of karst forming processes, coinciding with the base of the soluble carbonate rocks. Most caves are formed in limestone by dissolution. Caves can be classified in various other ways as well, including a contrast between active and relict: active caves have water flowing through them; relict caves do not, though water may be retained in them. Types of active caves include inflow caves ("into which a stream sinks"), outflow caves ("from which a stream emerges"), and through caves ("traversed by a stream"). Speleothems in Hall of the Mountain King of Ogof Craig a Ffynnon, a solutional cave in South Wales. Solutional Main article: Solutional cave Solutional caves or karst caves are the most frequently occurring caves. Such caves form in rock that is soluble; most occur in limestone, but they can also form in other rocks including chalk, dolomite, marble, salt, and gypsum. Rock is dissolved by natural acid in groundwater that seeps through bedding planes, faults, joints, and comparable features. Over time cracks enlarge to become caves and cave systems. The largest and most abundant solutional caves are located in limestone. Limestone dissolves under the action of rainwater and groundwater charged with H2CO3 (carbonic acid) and naturally occurring organic acids. The disso ------------------------------ Date: Mon, 19 Jul 2021 10:01:58 -0400 From: "One Day Bathroom Renovation" Subject: 24-Hour bathroom upgrade? 24-Hour bathroom upgrade? http://renovatomatic.us/vTKSA8BAClF9U0JqqwgbGQx02psCqfbg8X55diycFD_droDi http://renovatomatic.us/rm8MfN1J14SIUBj55RgliG8_C1oL7OPDRQh1xZ7JWSE95Nug sha, a street-bike racer, is travelling via auto with his friend to the airport. He spots the blurry outline of a woman trying to flag the auto down and gestures to her that it is already occupied. As he does, their fingers accidentally touch, and Harsha feels an electric current passing through him, which triggers a few fleeting images. After recovering from the shock, he flees the auto in search of the girl and inquires about her to a woman named Indira "Indu", unaware that Indu is the same woman. Indu, thinking he is stalking her, misdirects him by convincing him that the girl is her neighbour. She and her friends exploit Harsha, having him take them to places and promising that the girl will show. After Harsha beats up a group of men who were verbally harassing Indu, she starts to fall in love with him.Meanwhile, Indu's distant cousin Raghuveer lusts after her seeing her shape. He manipulates Indu and her father into trusting him. However, when he attempts to touch a sleeping Indu, he sees visions of a warrior slitting his throat. Raghuveer consults a tantrik, Ghora, who reveals that in a prior life, Raghuveer was a prince who lusted after Indu, and was killed by her lover, a warrior. Raghuveer is determined to find the reincarnation of the warrior and kill him. Meanwhile, Harsha discovers how Indu and her friends have been defrauding him, and after he pranks her in retaliation, they start to fall in love. Raghuveer discovers that Harsha is the reincarnation of the warrior, murders Indu's father, and frames Harsha. As Raghuveer and Indu leave in a helicopter, Harsha fails to catch them; falling into a lake, he faces a near-death experience and gets a full vision of his past-life in 1609.In 1609, Emperor Sher Khan is preparing to invade the kingdom of Udaigarh when he hears of the brave warrior Kala Bhairava (Harsha). King Vikram Singh's daughter, Princess Mithravindha Devi (Indu), loves Bhairava, but he holds himself back even though he reciprocates the same. Ranadev Billa (Raghuveer), the king's nep! hew and Mithra's cousin, lusts Mithra and plans a competition between himself and Bhairava; the winner will marry her and the loser will be banished from Udaigarh. Bhairava's victory leads to Ranadev's banishment. Vikram Singh, however, secretly requests that Bhairava not marry his daughter, because Bhairava has a high chance of dying in the ensuing battle with Khan's forces, and he does not wish to see Mithra widowed. 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X'YX'X4X*X1X'Y YY YX0Y X'YYX,YYX9X) YX%Y YX'Y X*YYY X1X3X'X&Y X'YX%YYX*X1YYY X) YYYX'X X#X1X3Y X1X3X'YX) X%YYX*X1YYY X) X%YY amanylolomklgkfjdh+unsubscribe@googlegroups.com. YX9X1X6 YX0Y X'YYYX'YX4X) X9YY X'YYY X(X X'YX*YY X%YY https://groups.google.com/d/msgid/amanylolomklgkfjdh/CAFRgcP2naLmrXWovbBHani7X6Sto8EbqHdjbD25VUv1S%2BWcG3g%40mail.gmail.com. ------------------------------ Date: Mon, 19 Jul 2021 12:46:44 +0200 From: "DroneX Pro" Subject: With Drone X Pro in your hand, you no longer need to look out for expensive cameras This email must be viewed in HTML mode. ------------------------------ End of alt.music.moxy-fruvous digest V14 #6987 **********************************************