Most Iapetian geological features are named after characters and locations in the Old French epic poem The Song of Roland , specifically the English translation by Dorothy L. Sayers. [1]
A mons /ˈmɒnz/ , pl. montes /ˈmɒntiːz/ , is a mountain.
Name | Coordinates | Diameter (km) | Approval Date | Namesake | Pronunciation | Refs |
---|---|---|---|---|---|---|
Carcassone Montes | 0°00′N216°42′W / 0.0°N 216.7°W | 740.0 | August 5, 2008 | Carcassonne, France | /kɑːrkəˈsoʊn/ | WGPSN |
Cordova Mons | 0°00′N206°12′W / 0.0°N 206.2°W | 85.0 | August 5, 2008 | Córdoba, Spain | /ˈkɔːrdoʊvə/ | WGPSN |
Gayne Mons | 0°00′N176°00′W / 0.0°N 176.0°W | 65.0 | August 5, 2008 | Gayne, Spain | WGPSN | |
Haltile Mons | 0°00′N190°24′W / 0.0°N 190.4°W | 45.0 | August 5, 2008 | Haltile, Spain | WGPSN | |
Seville Mons | 0°00′N346°18′W / 0.0°N 346.3°W | 69.0 | August 5, 2008 | Seville, Spain | /sɪˈvɪl/ | WGPSN |
Sorence Mons | 0°00′N193°42′W / 0.0°N 193.7°W | 46.0 | August 5, 2008 | Castle of Pinabel | WGPSN | |
Toledo Montes | 0°00′N136°00′W / 0.0°N 136.0°W | 1100.0 | August 5, 2008 | Toledo, Spain | /toʊˈliːdoʊ/ | WGPSN |
Tortelosa Montes | 0°00′N64°42′W / 0.0°N 64.7°W | 294.0 | August 5, 2008 | Tortelosa, Spain | WGPSN | |
Valterne Mons | 0°00′N170°36′W / 0.0°N 170.6°W | 50.0 | August 5, 2008 | Valterne, Spain | WGPSN |
There is one named Iapetian regio /ˈriːdʒioʊ/ (area of distinct albedo difference), Cassini:
Name | Coordinates | Diameter (km) | Approval Date | Namesake | Pronunciation | Refs |
---|---|---|---|---|---|---|
Cassini Regio | 28°06′S92°36′W / 28.1°S 92.6°W | 0 | 1982 | Giovanni Cassini, discoverer of Iapetus | /kəˈsiːnɪ/ | WGPSN |
There are two named Iapetian terrae /ˈtɛriː/ (large 'land' masses).
Name | Coordinates | Diameter (km) | Approval Date | Namesake | Pronunciation | Refs |
---|---|---|---|---|---|---|
Roncevaux Terra | 37°00′N239°30′W / 37.0°N 239.5°W | 1284.0 | 1982 | Battle of Roncevaux Pass | /rɒnsəˈvoʊ/ | WGPSN |
Saragossa Terra | 45°00′S180°00′W / 45.0°S 180.0°W | 2300.0 | August 5, 2008 | Saragossa, Spain | /særəˈɡɒsə/ | WGPSN |
The adjectival form of Roncevaux is Roncesvallian.
Named impact craters are:
Rhea is the second-largest moon of Saturn and the ninth-largest moon in the Solar System, with a surface area that is comparable to the area of Australia. It is the smallest body in the Solar System for which precise measurements have confirmed a shape consistent with hydrostatic equilibrium. It was discovered in 1672 by Giovanni Domenico Cassini.
In Greek mythology, Iapetus, also Japetus, is a Titan, the son of Uranus and Gaia and father of Atlas, Prometheus, Epimetheus, and Menoetius. He was also called the father of Buphagus and Anchiale in other sources.
Iapetus is the outermost of Saturn's large moons. With an estimated diameter of 1,469 km, it is the third-largest moon of Saturn and the eleventh-largest in the Solar System. Named after the Titan Iapetus, the moon was discovered in 1671 by Giovanni Domenico Cassini.
Hyperion, also known as Saturn VII, is the eighth-largest moon of Saturn. It distinguished by its highly irregular shape, chaotic rotation, low density, and its unusual sponge-like appearance. It was the first non-rounded moon to be discovered.
Phoebe is the most massive irregular satellite of Saturn with a mean diameter of 213 km (132 mi). It was discovered by William Henry Pickering on 18 March 1899 from photographic plates that had been taken by DeLisle Stewart starting on 16 August 1898 at the Boyden Station of the Carmen Alto Observatory near Arequipa, Peru. It was the first natural satellite to be discovered photographically.
The moons of Saturn are numerous and diverse, ranging from tiny moonlets only tens of meters across to the enormous Titan, which is larger than the planet Mercury. There are 146 moons with confirmed orbits, the most of any planet in the solar system. This number does not include the many thousands of moonlets embedded within Saturn's dense rings, nor hundreds of possible kilometer-sized distant moons that were seen through telescopes but not recaptured. Seven Saturnian moons are large enough to have collapsed into a relaxed, ellipsoidal shape, though only one or two of those, Titan and possibly Rhea, are currently in hydrostatic equilibrium. Three moons are particularly notable. Titan is the second-largest moon in the Solar System, with a nitrogen-rich Earth-like atmosphere and a landscape featuring river networks and hydrocarbon lakes. Enceladus emits jets of ice from its south-polar region and is covered in a deep layer of snow. Iapetus has contrasting black and white hemispheres as well as an extensive ridge of equatorial mountains among the tallest in the solar system.
The Iapetus Ocean was an ocean that existed in the late Neoproterozoic and early Paleozoic eras of the geologic timescale. The Iapetus Ocean was situated in the southern hemisphere, between the paleocontinents of Laurentia, Baltica and Avalonia. The ocean disappeared with the Acadian, Caledonian and Taconic orogenies, when these three continents joined to form one big landmass called Euramerica. The "southern" Iapetus Ocean has been proposed to have closed with the Famatinian and Taconic orogenies, meaning a collision between Western Gondwana and Laurentia.
This is a directory of lists of geological features on planets excepting Earth, moons and asteroids ordered by increasing distance from the Sun.
Roncevaux Terra is the name given to the northern part of the highly reflective side of Saturn's moon Iapetus. The southern half of this side is named Saragossa Terra. The other half of Iapetus, named Cassini Regio, is extremely dark. It is believed that Roncevaux Terra's colour is the underlying colour of Iapetus, while Cassini Regio was formed either by a substance that has covered up the brighter ice of the rest of the moon, or by a residue left from the sublimation of Roncevaux-type water ice.
The Caledonian orogeny was a mountain-building cycle recorded in the northern parts of the British Isles, the Scandinavian Caledonides, Svalbard, eastern Greenland and parts of north-central Europe. The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490–390 million years ago (Ma). It was caused by the closure of the Iapetus Ocean when the Laurentia and Baltica continents and the Avalonia microcontinent collided.
Turgis is the largest known crater on Saturn's moon Iapetus. It is 580 km in diameter, 40% of the moon's diameter and one of the larger craters in the Solar System. It is named after a Saracen baron, Turgis of Turtelose (Tortosa).
The Iapetus Suture is one of several major geological faults caused by the collision of several ancient land masses forming a suture. It represents in part the remains of what was once the Iapetus Ocean. Iapetus was the father of Atlas in Greek mythology, making his an appropriate name for what used to be called the 'Proto-Atlantic Ocean'. When the Atlantic Ocean opened, in the Cretaceous period, it took a slightly different line from that of the Iapetus suture, with some originally Laurentian rocks being left behind in north-west Europe and other, Avalonian, rocks remaining as part of Newfoundland.
Mons 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.
The following outline is provided as an overview of and topical guide to Saturn:
Abisme /æˈbiːm/ is located in Cassini Regio at 37.9°N 267.1°E. Craters Climborin, Clarin, Dapamort, Johun and Valdebron can be found inside Abisme. It was imaged for the first time by the Cassini spacecraft in 2004.