"Angeles' Hollywood Bowl. The verses include musical references such as ""Silly Willy with the Philly band"" and Jimmy Page's guitar, and the Rainbow Theatre. In addition to the normal Wings line-up, Allen Toussaint played piano on this song. ""Rock Show"" is in the key of A major. A major is the dominant key of D major, the key of ""Venus and Mars"". ""Venus and Mars"" ""Rock Show"" ""Hand Bells are only played on the album version"" (Credits from 2014 Deluxe ""Venus and Mars"" Remaster) ""Venus and Mars"" also has a reprise that appears on the ""Venus and Mars"" album, which"
"Maxwell Montes Maxwell Montes is a mountain massif on the planet Venus, of which a peak (Skadi Mons) is the highest point on the planet's surface. Located on Ishtar Terra, the more northern of the planet's two major highlands, Maxwell Montes is high. It rises about 6.4 kilometers above and to the east (21,000 ft above, and 4 miles to the east) of Lakshmi Planum, and is about long by wide. The western slopes are very steep, whereas the eastern slopes descend gradually into Fortuna Tessera. Due to its elevation it is the coolest (about ) and least pressurised (about"
"mountain belts unit is the only real mountain range on Venus in the area surrounding Lakshmi Planum, which covers only 1.3 x 10 km of the Venusian global surface, while involves structural deformation of different materials in their formation. There are in total four major mountain belts mapped on Venus, including the belts of Danu Montes, Akna Montes, Freyje Montes and Maxwell Montes (the highest mountain on Venus with elevation of around 12 km). When looking at the cross-cutting relationship, the inner ridges of the belts seems to be embayed by the material of regional plains (pr), which covered the"
"the four main mountain ranges of Venus: Maxwell Montes on the eastern edge, Freyja Montes in the north, Akna Montes on the western edge, and Danu Montes in the southern region. These surround the lower plain of Ishtar Terra, which is named Lakshmi Planum (named after the Hindu goddess Lakshmi). Ishtar Terra also contains volcanoes named after famous women: Sacajawea, Colette, and Cleopatra. Ishtar Terra is also the site of many tesserae, formed by tectonic deformation. Ishtar Terra Ishtar Terra is one of two main highland regions on the planet Venus. It is the smaller of the three ""continents"", and"
"Venus, possible. Maxwell Montes, Alpha Regio, and Beta Regio are the three exceptions to the rule that the surface features of Venus are to be named for females. The name, originally given by Ray Jurgens in 1970 on the urging of Tommy Gold, was approved by the International Astronomical Union's Working Group for Planetary System Nomenclature (IAU/WGPSN) between 1976 and 1979. Maxwell Montes Maxwell Montes is a mountain massif on the planet Venus, of which a peak (Skadi Mons) is the highest point on the planet's surface. Located on Ishtar Terra, the more northern of the planet's two major highlands,"
"Montes (7 km, 4.3 mi). Despite the relatively flat landscape of Venus, the altimetry data also found large inclined plains. Such is the case on the southwest side of Maxwell Montes, which in some parts seems to be inclined some 45°. Inclinations of 30° were registered in Danu Montes and Themis Regio. About 75% of the surface is composed of bare rock. Based on altimeter data from the ""Pioneer Venus"" probe, supported by 'Magellan' data, the topography of the planet is divided into three provinces: lowlands, deposition plains, and highlands. This unit covers about 10% of the planet's surface, with"
"Hellespontus Montes The Hellespontus Montes is a mountain range on Mars. It stretches 711 km and nearly runs north to south. It is in the Noachis quadrangle and the southeasternmost area of Noachis Terra, and is located midway between the highland area of Noachis and Hellas Planitia, an impact basin which has the planet's lowest point, that basin is east of the ranges. The mountains are named after a Classical albedo feature. Its name was approved in 1973, by the International Astronomical Union (IAU) Working Group for Planetary System Nomenclature. Its highest point is located around the middle at an"
"round mountains found on Venus get names with the term ""farrum"". The term ""mons"", like other terms of planetary nomenclature, describes only the external view of the feature, but not its origin or geological structure. It is used for mountains of any origin, and objects in this class are very diverse. Usually they are results of tectonic, impact or volcanic processes. Examples of such mountains are the Maxwell Montes on Venus, the Montes Apenninus on the Moon and Olympus Mons on Mars, respectively. More unusual origins are also possible. For example, the Geryon Montes of Mars are an erosional remnant"
"Egypt Mons Egypt Mons is a mountain on Jupiter's moon Io. It is 10 kilometers in height, making it the 11th tallest mountain on Io, and taller than Mount Everest. Although the U.S. Geological Survey gives a diameter of 193.7 kilometers, the Io Mountain Database gives a length of 133.8 kilometers and a width of 146.0 kilometers. It is a Flatiron Massif mountain, meaning it has a rugged, irregular appearance and complex surface morphology. It is 9792 km in area and located at . It has a steep, north-facing scarp. Egypt Mons is named for Egypt, because that is the"
"lithospheric loading by dense stacks of volcanic lavas, as suggested for those of the lunar maria. The surface of Venus is comparatively very flat. When 93% of the topography was mapped by ""Pioneer Venus"", scientists found that the total distance from the lowest point to the highest point on the entire surface was about 13 kilometres (8 mi), while on the Earth the distance from the basins to the Himalayas is about 20 kilometres (12.4 mi). According to the data of the altimeters of the ""Pioneer"", nearly 51% of the surface is found located within 500 metres (1,640 ft) of"
"Olympus Mons Olympus Mons (; Latin for Mount Olympus) is a very large shield volcano on the planet Mars. The volcano has a height of nearly 25 km (13.6 mi or 72,000 ft) as measured by the Mars Orbiter Laser Altimeter (MOLA). Olympus Mons is about two and a half times Mount Everest's height above sea level. It is the largest volcano, the tallest planetary mountain, and the second tallest mountain in the Solar System compared to Rheasilvia on Vesta. It is the youngest of the large volcanoes on Mars, having formed during Mars's Hesperian Period. It had been known"
"Mars are very similar to the shield volcanoes on Earth. Both have gently sloping flanks, collapse craters along their central structure, and are built of highly fluid lavas. Volcanic features on Mars were observed long before they were first studied in detail during the 1976–1979 Viking mission. The principal difference between the volcanoes of Mars and those on Earth is in terms of size; Martian volcanoes range in size up to high and in diameter, far larger than the high, wide Hawaiian shields. The highest of these, Olympus Mons, is the tallest known mountain on any planet in the solar"
"Tartarus Montes The Tartarus Montes are a mountain range on the planet Mars, stretching over 1070 km and located around the coordinates 15.46º N, 167.54º E, between Orcus Patera and the Elysium volcanic region. Albedo was first identified from the contrast of bright and dark signals photographed by Eugène Antoniadi. The mountain range was named in 1885. It has been named after Greek deity of the underworld, Tartarus, by the standard planetary nomenclature for Martian landforms. According to Greek myth, Tartarus is the lowest part of Hades. Zeus imprisoned the Titans in Tartarus. The second part of the name ""Montes"""
"on the Moon, 23 on Io, 13 on Titan, 9 on Iapetus, 1 on Mercury and 1 on Tethys. They are named differently on different celestial bodies: Mons (planetary nomenclature) Mons (plural: montes, from the Latin word for ""mountain"") is a mountain on a celestial body. The term is used in planetary nomenclature: it is a part of the international names of such features. It is capitalized and usually stands after the proper given name, but stands before it in the case of lunar mountains (for example, there is a Martian mountain Arsia Mons and a lunar mountain Mons Argaeus)."
"rock stronger and helps preserve surface features. The features observed provide evidence for the geological processes at work. Twenty feature types have been categorized thus far. These classes include local features, such as craters, coronae, and undae, as well as regional-scale features, such as planitiae, plana, and tesserae. Plains are large areas of relatively flat topography on Venus that form at varying elevations. Plains with elevations within 1–3 km of the datum are referred to as lowland plans, or ""planitiae"", and those above are named highland plains, or ""plana"". Plains cover 80% of the Venusian surface, and, unlike those seen"
"fully contains the feature. Terra Nivium Terra Nivium (Latin for ""Land of Snows"") is a roughly triangular highland region on the Moon. In his ""Almagestum novum"", the notable selenographer Giovanni Riccioli named the various highland regions terrae. However, unlike his naming scheme for craters and lunar maria, his nomenclature for the continental areas of the Moon never came into common use. It lies to the north of the Mare Vaporum and is bounded along the northwest by the rugged Montes Apenninus range, and to the northeast by the less impressive Montes Haemus mountains. Portions of this area have been penetrated"
"and Elysium. Each province contains a series of giant shield volcanoes that are similar to what we see on Earth and likely are the result of mantle hot spots. The surfaces are dominated by lava flows, and all have one or more collapse calderas. Mars has the largest volcano in the Solar System, Olympus Mons, which is more than three times the height of Mount Everest, with a diameter of 520 km (323 miles). The summit of the mountain has six nested calderas. Because there is no plate tectonics on Venus, heat is mainly lost by conduction through the lithosphere."
"returned images of a surface covered in sediment and relatively angular rocks. The surface was mapped in detail by ""Magellan"" in 1990–91. The ground shows evidence of extensive volcanism, and the sulfur in the atmosphere may indicate that there have been some recent eruptions. About 80% of the Venusian surface is covered by smooth, volcanic plains, consisting of 70% plains with wrinkle ridges and 10% smooth or lobate plains. Two highland ""continents"" make up the rest of its surface area, one lying in the planet's northern hemisphere and the other just south of the equator. The northern continent is called"
"time. This section introduces several of the larger physiographic regions of Mars. Together, these regions illustrate how geologic processes involving volcanism, tectonism, water, ice, and impacts have shaped the planet on a global scale. The northern and southern hemispheres of Mars are strikingly different from each other in topography and physiography. This dichotomy is a fundamental global geologic feature of the planet. Simply stated, the northern part of the planet is an enormous topographic depression. About one-third of the planet’s surface (mostly in the northern hemisphere) lies 3–6 km lower in elevation than the southern two-thirds. This is a first-order"
"Pavonis Mons Pavonis Mons (Latin for ""peacock mountain"") is a large shield volcano located in the Tharsis region of the planet Mars. It is the middle member of a chain of three volcanic mountains (collectively known as the Tharsis Montes) that straddle the Martian equator between longitudes 235°E and 259°E. The volcano was discovered by the Mariner 9 spacecraft in 1971 and was originally called Middle Spot. Its name formally became Pavonis Mons in 1973. The equatorial location of its peak and its height make it the ideal terminus for a space elevator, and it has often been proposed as"
"Ishtar Terra Ishtar Terra is one of two main highland regions on the planet Venus. It is the smaller of the three ""continents"", and is located near the north pole. It is named after the Akkadian goddess Ishtar. The size of Ishtar Terra is roughly between the sizes of Australia and the continental United States. On its eastern edge lies the great mountain chain Maxwell Montes, which is 11 km high, compared to Mt. Everest at 8.8 km. On one side of the mountain chain is an impact crater of 100 km in diameter filled with lava. Ishtar Terra contains"
"Mount Everest and about as big in area as all of Europe. Tharsis contains a group of large volcanoes. Olympus Mons is the tallest. Tharsis is a land of great volcanoes. Olympus Mons is the tallest known volcano in the Solar System; it is 100 times larger than any volcano on Earth. Ascraeus Mons and Pavonis Mons are at least 200 miles across and are over six miles above the plateau that they sit on—and, the plateau is three to four miles above the zero altitude of Mars. Pavonis Mons, the middle in a line of three volcanoes, sits at"
"Maat Mons Maat Mons is a massive shield volcano. It is the second-highest mountain, and the highest volcano, on the planet Venus. It rises above the mean planetary radius at , and nearly 5 km above the surrounding plains. It is named after the Egyptian goddess of truth and justice, Ma'at. Maat Mons has a large summit caldera, 28×31 km in size. Within the large caldera there are at least five smaller collapse craters, up to 10 km in diameter. A chain of small craters 3–5 km in diameter extends some 40 km along the southeast flank of the volcano,"
"place where Io ended her wanderings in the mythology. Its name was adopted by the International Astronomical Union in 1997. To the northwest is Babbar Patera, and southeast is Hermes Mensa. Svarog Patera can be found to the southwest. Egypt Mons Egypt Mons is a mountain on Jupiter's moon Io. It is 10 kilometers in height, making it the 11th tallest mountain on Io, and taller than Mount Everest. Although the U.S. Geological Survey gives a diameter of 193.7 kilometers, the Io Mountain Database gives a length of 133.8 kilometers and a width of 146.0 kilometers. It is a Flatiron"
"tallest mountain known in the Solar System is in Rheasilvia crater on the asteroid Vesta, which contains a central mound that rises high; Olympus Mons on Mars is nearly the same height, at high. In comparison, Mount Everest rises to altitude above sea level (asl), but is only (base-to-peak) (btp). Africa's Mount Kilimanjaro is about altitude above sea level to the Uhuru peak; also 4.6 km base-to-peak. America's Denali, also known as ""Mount McKinley"", has a base-to-peak of . The Franco-Italian ""Mont Blanc/Monte Bianco"" is in altitude above sea level, Mount Fuji, which overlooks Tokyo, Japan, is about altitude. Compared"
"this, there are far fewer craters on Mars compared with the Moon, because the atmosphere of Mars provides protection against small meteors and surface modifying processes have erased some craters. Martian craters can have a morphology that suggests the ground became wet after the meteor impacted. The shield volcano Olympus Mons (""Mount Olympus"") is an extinct volcano in the vast upland region Tharsis, which contains several other large volcanoes. Olympus Mons is roughly three times the height of Mount Everest, which in comparison stands at just over . It is either the tallest or second-tallest mountain in the Solar System,"
"Venus"" or ""mons veneris"" is derived from Latin for ""mound of Venus"". Although not part of external genitalia itself, the pubic mound can be regarded as an erogenous zone and is highly eroticized in many cultures. Throughout history, the complete or partial removal of pubic hair has been common in many societies, and more recently it has become widespread in the Western world. The full removal of pubic hair by use of wax, sugar or shaving, known as ″Brazilian wax″, has become common practice in recent years. In some circumstances, the mons veneria is subjected to aesthetic ideals beyond hair"
"Mons pubis In human anatomy, and in mammals in general, the mons pubis (pubic mound, also known simply as the mons, and known specifically in females as the mons Venus or mons veneris), is a rounded mass of fatty tissue found over the pubic symphysis of the pubic bones. For women and girls, the mons pubis forms the anterior portion of the vulva. It divides into the labia majora (literally ""larger lips""), on either side of the furrow known as the pudendal cleft, that surrounds the labia minora, clitoris, urethra, vaginal opening, and other structures of the vulval vestibule. The"
"Dimples of Venus The dimples of Venus (also known as back dimples, butt dimples or Venusian dimples) are sagittally symmetrical indentations sometimes visible on the human lower back, just superior to the gluteal cleft. They are directly superficial to the two sacroiliac joints, the sites where the sacrum attaches to the ilium of the pelvis. The term ""dimples of Venus"", while informal, is a historically accepted name within the medical profession for the superficial topography of the sacroiliac joints. The Latin name is ""fossae lumbales laterales"" (""lateral lumbar indentations""). These indentations are created by a short ligament stretching between the"
"Plato (crater) Plato is the lava-filled remains of a lunar impact crater on the Moon. It is located on the northeastern shore of the Mare Imbrium, at the western extremity of the Montes Alpes mountain range. In the mare to the south are several rises collectively named the Montes Teneriffe. To the north lies the wide stretch of the Mare Frigoris. East of the crater, among the Montes Alpes, are several rilles collectively named the Rimae Plato. The exact elevation was first mapped on an LTO map. Its widest diameter is 109 km long and the depth is 1 km."
"to Svarog and Viracocha Paterae has been suggested to be evidence for a structural relationship between mountains and calderas on Io. Silpium Mons Silpium Mons is a mountain on Jupiter's moon Io. It is 5.6 kilometers in height, 113 kilometers in length, and 79.7 kilometers in width. It covers an area of 7073 km. It is a striated ridge, meaning it is an elevated structure dominated by one or more prominent linear or arcurate rises. It is named after a location in Greece where the mythological Io died of grief. Its name was adopted by the International Astronomical Union in"
"elevation of about 1,500 m, about 10 km higher than the lowest point of the planet located northeast but about 3,000 m lower than the highlands towards the west.. West of the ranges are Rabe and Matara craters. Hellespontus Montes The Hellespontus Montes is a mountain range on Mars. It stretches 711 km and nearly runs north to south. It is in the Noachis quadrangle and the southeasternmost area of Noachis Terra, and is located midway between the highland area of Noachis and Hellas Planitia, an impact basin which has the planet's lowest point, that basin is east of the"
"in the heavens. According to Aristotle, along with Plato, the number of levels of the heavens was at least eight, which included Saturn, Venus, Mercury, Jupiter, Mars, the Sun, the Moon, and the stars. du Chevreul had a different theory in which he counted only five levels: Saturn, Jupiter, Mars, the Sun, and the Moon. Unlike his predecessors who either argued that Venus and Mercury were above the Sun or below it, du Chevreul asserted all of the above. Since Venus and Mercury orbit the Sun, du Chevreul deduced, they could be found both above and below it. Thus, Venus"