خطای عبارت: نویسه نقطهگذاری شناخته نشده «۵» quadrangle]]
کوه ائولیس، همچنین غیررسمی به عنوان کوه شارپ شناخته می شود، یک کوه در مریخ است که در مرکز گودال گیل سربرافراشته است. ارتفاع این کوه از کف گودال گیل بیش از ۵.۵ کیلومتر است.
Mount Sharp, officially Aeolis Mons ( IPA: ), is a [ˈiːəlɨs ˈmɒnz] mountain on Mars. It forms the central peak within Gale crater and is located around , rising 5.5 km (18,000 ft) high from the valley floor. It has the ID of 15,000 in the 5°05′S 137°51′E / 5.08°S 137.85°E Gazetteer of Planetary Nomenclature from the US Geological Survey.
On August 6, 2012,
(the Curiosity Mars Science Laboratory rover) landed in "Yellowknife" Quad 51    of  Aeolis Palus, next to the mountain. NASA named the landing site  Bradbury Landing on August 22, 2012. Aeolis Mons is a primary goal for scientific study.  On June 5, 2013, NASA announced that  Curiosity would begin an 8 km (5.0 mi) journey from the Glenelg area to the base of Aeolis Mons. On November 13, 2013, NASA announced that an entryway would traverse on its way to Aeolis Mons was to be named "Murray Buttes", in honor of Curiosity planetary scientist Bruce C. Murray (1931–2013). The trip was expected to take about a year and would include stops along the way to study the local terrain.   
On September 11, 2014, NASA announced that the
had reached Aeolis Mons, the rover mission's long-term prime destination. Curiosity rover 
On October 5, 2015, possible
recurrent slope lineae, wet brine flows, were reported on Mount Sharp near Curiosity.
On June 1, 2017, NASA reported that an ancient
striated lake had existed in Gale crater that could have been favorable for microbial life.  
As of June 26, 2019,
Curiosity has been on the planet Mars for 2448 sols (2515 days) since landing on August 6, 2012. (See
The mountain appears to be an enormous mound of eroded sedimentary layers sitting on the central peak of Gale. It rises 5.5 km (18,000 ft) above the northern crater floor and 4.5 km (15,000 ft) above the southern crater floor, higher than the southern crater rim. The sediments may have been laid down over an interval of 2 billion years,
and may have once completely filled the crater. Some of the lower sediment layers may have originally been deposited on a lake bed,  while observations of possibly cross-bedded strata in the upper mound suggest  aeolian processes. However, this issue is debated,   and the origin of the lower layers remains unclear.  If  katabatic wind deposition played the predominant role in the emplacement of the sediments, as suggested by reported 3 degree radial slopes of the mound's layers, erosion would have come into play largely to place an upper limit on the mound's growth. 
On December 8, 2014, a panel of NASA scientists discussed (
archive 62:03) the latest observations of Curiosity about how water may have helped shape the landscape of Mars, including Aeolis Mons, and had a climate long ago that could have produced long-lasting lakes at many Martian locations.  
On October 8, 2015, NASA confirmed that lakes and streams existed in
Gale crater 3.3 - 3.8 billion years ago delivering sediments to build up the lower layers of Mount Sharp. 
On February 1, 2019, NASA scientists
reported that the Mars determined, for the first time, the Curiosity rover density of Mount Sharp in Gale crater, thereby establishing a clearer understanding of how the mountain was formed. 
Aeolis Mons is 5.5 km (18,000 ft) high, about the same height as
Mons Huygens, the tallest lunar mountain, and taller than Mons Hadley visited by Apollo 15. The tallest mountain known in the Solar System is in Rheasilvia crater on the asteroid Vesta, which contains a central mound that rises 22 km (14 mi; 72,000 ft) high; Olympus Mons on Mars is nearly the same height, at 21.9 km (13.6 mi; 72,000 ft) high.
Mount Everest rises to 8.8 km (29,000 ft) altitude above sea level (asl), but is only 4.6 km (15,000 ft) (base-to-peak) (btp). Africa's  Mount Kilimanjaro is about 5.9 km (19,000 ft) 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 5.5 km (18,000 ft).
The Franco-Italian  is 4.8 km (16,000 ft) in altitude above sea level, Mont Blanc/Monte Bianco   Mount Fuji, which overlooks Tokyo, Japan, is about 3.8 km (12,000 ft) altitude. Compared to the Andes, Aeolis Mons would rank outside the hundred tallest peaks, being roughly the same height as Argentina's Cerro Pajonal; the peak is higher than any above sea level in Oceania, but base-to peak it is considerably shorter than Hawaii's Mauna Kea and its neighbors.
Discovered in the 1970s,
In March 2012, NASA unofficially named it "Mount Sharp", after American geologist  Robert P. Sharp. 
the mountain remained unnamed for several decades. When Gale crater became a candidate landing site, the mountain was given various labels e.g. in 2010 a NASA photo caption called it "Gale crater mound".
Mount Sharp (Aeolis Mons)
to the sizes of three large mountains on Earth.
Since 1919 the
International Astronomical Union (IAU) has been the official body responsible for planetary nomenclature. Under its long-established rules for naming features on Mars, mountains are named after the Classical albedo feature in which they are located, not after people. In May 2012 the IAU officially named the mountain Aeolis Mons after the Aeolis albedo feature. It also gave the name  Aeolis Palus to the plain located on the crater floor between the northern wall of Gale and the northern foothills of the mountain.    The IAU's choice of name is supported by the  United States Geological Survey. Martian craters are named after deceased scientists, so in recognition of NASA and Sharp, at the same time the IAU named "  Robert Sharp", a large (150 km (93 mi) diameter), crater located about 260 km (160 mi) west of Gale.
NASA and the
European Space Agency continue to refer to the mountain as "Mount Sharp" in press conferences and press releases. This is similar to their use of other informal names, such as the  Columbia Hills near one of the Mars Exploration Rover landing sites.
In August 2012, the magazine
ran an article explaining the rationale of the two names and held an informal poll to determine which one was preferred by their readers. Over 2700 people voted, with Aeolis Mons winning by 57% to Mount Sharp's 43%. Sky & Telescope
Curiosity rover explores Mount Sharp (15 May 2019)
On December 16, 2014, NASA reported detecting, based on measurements by the
Curiosity rover, an unusual increase, then decrease, in the amounts of methane in the atmosphere of the planet Mars; as well as, detecting Martian organic chemicals in powder drilled from a rock by the . Also, based on Curiosity rover deuterium to hydrogen ratio studies, much of the water at Gale Crater on Mars was found to have been lost during ancient times, before the lakebed in the crater was formed; afterwards, large amounts of water continued to be lost.  
On June 1, 2017, NASA reported that the
Curiosity rover provided evidence of an ancient lake in Gale crater on Mars that could have been favorable for microbial life; the ancient lake was stratified, with shallows rich in oxidants and depths poor in oxidants; and, the ancient lake provided many different types of microbe-friendly environments at the same time. NASA further reported that the will continue to explore higher and younger layers of Mount Sharp in order to determine how the lake environment in ancient times on Mars became the drier environment in more modern times. Curiosity rover  
On August 5, 2017, NASA celebrated the fifth anniversary of the
landing, and related exploratory accomplishments, on the planet Curiosity rover mission Mars.  (Videos:  ; Curiosity 's First Five Years (02:07) ; Curiosity 's POV: Five Years Driving (05:49) )
Curiosity 's Discoveries About Gale Crater (02:54)
On April 11, 2019, NASA announced that the
on the planet Curiosity rover Mars drilled into, and closely studied, a " clay-bearing unit" which, according to the rover Project Manager, is a "major milestone" in Curiosity 's journey up Mount Sharp.
Curiosity at Mount Sharp
Self-portrait of the
rover at the Mojave site (January 31, 2015). Curiosity
As of June 26, 2019,
Curiosity has been on the planet Mars for 2448 sols (2515 total days; ) since landing on August 6, 2012. Since September 11, 2014, 6 years, 324 days Curiosity has been exploring the slopes of Mount Sharp,  where more information about the  history of Mars is expected to be found. As of late January 2019, the rover has traveled over 20.05 km (12.46 mi) and climbed over 327 m (1,073 ft) in elevation    to, and around, the mountain base since landing at "  Bradbury Landing" in August 2012. 
Credit: NASA/JPL-Caltech/University of Arizona
Curiosity rover (center bright blue) on Mount Sharp viewed from space ( MRO; HiRISE; June 5, 2017). 
Overview map - blue oval marks "Base of Aeolis Mons" (August 17, 2012).
Traverse map - route from
Landing to slopes on Aeolis Mons (September 11, 2014).
Close-up Map - new route (yellow) - Aeolis Mons slopes (September 11, 2014).
Close-up map - new route (yellow) - Aeolis Mons slopes (September 11, 2014).
Close-up map - Aeolis Mons slopes - with few craters (bottom) (September 11, 2014).
Geology map - Aeolis Mons slopes (September 11, 2014).
Geology map - Aeolis Mons slopes (September 11, 2014).
"Murray Buttes" knobs - Aeolis Mons slopes (November 13, 2013).
"Murray Buttes" mesa - Aeolis Mons slopes (September 11, 2014).
"Murray Formation" bands - Aeolis Mons slopes (September 11, 2014).
"Pahrump Hills" - Notable places at base of Aeolis Mons (Autumn, 2014).
sand - viewed by Curiosity (November 13, 2014).
sand - Curiosity 's tracks (November 7, 2014).
bedrock on Mars - viewed by Curiosity (November 9, 2014).
rock outcrop on Mars - viewed by Curiosity (October 7, 2014).
bedrock on Mars - viewed by Curiosity (November 23, 2014).
Ancient Lake fills Gale Crater on Mars (simulated view).
Murray formation lakebeds with aeolian(?) erosional fins, October 9, 2016
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Look up in Wiktionary, the free dictionary. Aeolis Mons