Question

Which is the highest mountain in the solar system and where is it?

Answer 1

Hint: It is an enormous shield spring of gushing lava on the planet Mars. The well of lava has a statue of more than 21 km ($13.6$ mi or 72,000 ft) as estimated by the Mars Orbiter Laser Altimeter (MOLA). It is also called Mount Olympus.

Complete step-by-step solution:
Olympus Mons is a huge shield well of lava on the planet Mars. The fountain of liquid magma has a statue of more than 21 km as estimated by the Mars Orbiter Laser Altimeter (MOLA). Olympus Mons is around over multiple times Mount Everest's stature above ocean level. It is one of the biggest volcanoes, the tallest planetary mountain, and the second tallest mountain at present found in the Solar System, tantamount to Rheasilvia on Vesta. It is regularly referred to as the biggest spring of gushing lava in the Solar System. Nonetheless, by certain measurements, different volcanoes are significantly bigger. Alba Mons, upper east of Olympus Mons, has approximately multiple times the surface zone, yet is just around $33\mathrm{\%}$ the tallness. Pele, the biggest known fountain of liquid magma on Io, is additionally a lot bigger, at around multiple times the surface territory, yet is significantly complimented. Moreover, Tharsis Rise, a huge volcanic structure on Mars of which Olympus Mons is a section, has been deciphered as a tremendous spreading of lava. On the off chance that this is affirmed, Tharsis would be by a long shot the biggest fountain of liquid magma in the Solar System. Olympus Mons is the most youthful of the huge volcanoes on Mars, having framed during Mars' Hesperian Period. It had been known to cosmologists since the late nineteenth century as the albedo included Nix Olympica (Latin for "Olympic Snow"). Its rugged nature was presumed a long time before space tests affirmed its way of life as a mountain. The well of lava is situated in Mars' western side of the equator, with the middle at ${18}^{\circ }{39}^{\prime }\text{N }{226}^{\circ }{12}^{\prime }\text{E}$, simply off the northwestern edge of the Tharsis swell. The western bit of the spring of gushing lava lies in the Amazonis quadrangle (MC-8) and the focal and eastern bits in the bordering Tharsis quadrangle (MC-9). Two effect holes on Olympus Mons have been relegated to temporary names by the International Astronomical Union. They are the $15.6$ km ($9.7$mi)- breadth Korzok hole (${18}^{\circ }{25}^{\prime }\text{N}{228}^{\circ }{05}^{\prime }\text{E}$) and the $10.4$ km ($6.5$ mi)- the distance across Pangboche hole (${17}^{\circ }{10}^{\prime }\text{N }{226}^{\circ }{25}^{\prime }\text{E}$). The pits are eminent for being two of a few presumed source regions for shergottites, the most plentiful class of Martian shooting stars. Olympus Mons is the most noteworthy mountain in the close planetary system. This mountain is found on Mars, it is multiple times taller than Mount Everest simultaneously this mountain is exceptionally wide and covers an enormous territory. This mountain is around 24 km long.

Note: Olympus Mons is the consequence of a large number of exceptionally liquid, basaltic magma streams that poured from volcanic vents throughout a significant stretch of time.