Blogs

  • News
  • |
  • Art
  • |
  • History
  • |
  • Food and Travel
  • |
  • Science
Dinosaur Tracking

Where paleontology meets pop culture

Hominid Hunting

Meet the members of the tangled human family tree

Innovations

How human ingenuity is changing the way we live

Surprising Science

Ideas, news and discoveries from the world of science


January 9, 2012

The Tallest Mountains in the Solar System

Mauna Loa (as seen from nearby Mauna Kea) is tall enough to have snow, at least when the volcano isn't erupting (courtesy of flickr user superfluity)

If asked to name the tallest mountain on Earth, most people would answer Mount Everest. They’d be wrong–Everest is the highest peak on the planet, but mountains are measured from their base to their peak, and Everest’s base sits far above sea level on the Tibetan Plateau. And when you start looking at the tallest (known) mountains in the solar system, Mount Everest, at only 2.3 to 2.9 miles tall (depending on where you decide the mountain’s base is located), doesn’t even make the list:

(1) Olympus Mons - 15.5 miles
The largest volcano on Mars is also the solar system’s tallest mountain. Measuring 374 miles in diameter, it covers about the same amount of land as the state of Arizona. Olympus Mons is located near three other volcanoes known as the Tharsis Montes. The volcanoes in this area are all 10 to 100 times bigger than Earth’s largest volcanoes. They can get this big because, unlike on Earth, there are no plate tectonics on Mars that can drag a volcano away from its hotspot–they just sit in one volcanically active place and grow bigger and bigger.

(2) Rheasilvea Mons – 13.2 miles
Rheasilvea, on the asteroid Vesta, sits at the center of a 300-mile wide crater. The asteroid is currently the subject of a close study by the spacecraft Dawn, which will continue to circle it through the first half of 2012 before moving on for a rendezvous with the asteroid Ceres in 2015. Rheasilvea Mons sometimes gets named the tallest peak in the solar system, but even with satellites and spacecraft monitoring faraway planets, moons and asteroids, measuring these things is rather difficult (which should explain why the numbers for heights given here may differ from what you’ve seen elsewhere–sources often disagree).

(3) Equatorial Ridge of Iapetus – 12.4 miles
Saturn’s moon of Iapetus has a couple of weird features. The first is a huge crater that gives the moon the appearance of the Death Star from Star Wars. The second is an equatorial ridge, with some peaks reaching over 12 miles high, that makes Iapetus look like a walnut. Scientists aren’t quite sure how the ridge formed, but they have hypothesized that it was either the remnant of the moon’s earlier oblate shape, icy material pushed up from beneath the moon’s surface or even the remainder of a collapsed ring.

(4) Ascreaus Mons – 11.3 miles
This volcano on Mars is the tallest of the three volcanoes known as the Tharsis Montes, which appear in a straight line near Olympus Mons. Ascreaus Mons has a central caldera that is 2.1 miles deep. It was first spotted by the Mariner 9 spacecraft in 1971 and then named the North Spot, as it appeared as a spot in a dust storm photographed by the spacecraft. Later images revealed it was a volcano and the spot was remaned.

(5) Boösaule Montes – 10.9 miles
Boösaule Montes is a collection of three mountains on Io, a moon of Jupiter, all connected by a raised plain. The mountain termed “South” is the tallest of the three. One side of the mountain has such a steep slope, 40 degrees, that scientists think that it was the site of a huge landslide.

(6) Arsia Mons – 9.9 miles
This is second tallest volcano from the Tharsis Montes on Mars. Based on the discovery of certain geological features on the volcano, scientists think that Arsia Mons may be home to glaciers.

(7) Pavonis Mons – 8.7 miles
Pavonis Mons is the shortest of the three volcanoes that make up the Tharsis Montes, and it has also been suggested to be home to glaciers.

(8) Elysium Mons - 7.8 miles
This Martian volcano is a big fish in a little pond, metaphorically speaking. It is the tallest volcano in the Elysium Planitia, a region in Mars’ Eastern Hemisphere that is the second largest volcanic system on the planet.

(9) Maxwell Montes - 6.8 miles
This mountain range on Venus stretches for 530 miles. Scientists aren’t sure how the mountains formed, but they think they are home to large amounts of fool’s gold (iron pyrite).

(10) Mauna Loa – 5.7 miles
Earth just squeaks into this top ten list with this active volcano on the island of Hawaii (remember, mountains are measured from their base to their peak, and Mauna Loa’s base is far beneath the ocean surface). Mauna Loa is one of many active and dormant volcanoes created by a hotspot beneath the Pacific Ocean plate. As the plate moves over the hotspot, which has been active for at least 30 million years, new islands begin to form and old ones, no longer being built up through volcanic activity, whither wither away.



***

Sign up for our free email newsletter and receive the best stories from Smithsonian.com each week.

9 Comments »

  1. Bodhipaksa says:

    Sorry to be a pedant, but it’s “wither away” rather than “whither away.”

    Enjoyed the article.

    There’s no need to publish this comment.

  2. Sarah Zielinski says:

    Usually people are really kind of nasty when they spot a mistake like this and point it out. But you’re so nice about it, I had to publish it despite your request. (Oh, and thanks for noting it–now I know and probably won’t make that mistake again.)

  3. Chris Landau says:

    As this site is now tracking English grammar and geological terminology, let us change wither to weather as wither implies that the mountain is alive, as in, “a plant withers in the scorching sun.” If the intention here is to imply that Mars, the God of War is dying on Mars, then wither is fine. We can not use Gaia as this is not Earth. So whether you believe it or not, or whither you choose a new route to test a new theory, the important point that the article brings up to be answered is,”Why are the mountains where they are and why are they so tall and what does it all mean and what would change if they were not there?” Let me know.

  4. Guernican says:

    At the risk of compounding the pedantry, and fully recognising that this is a subsidiary rather than central point, I’d tend to agree with Chris. “Wither” implies the wasting away of a living organism.

  5. Luka says:

    Please correct me if I’m wrong, but as far as I’m familiar with mountain measuring, Mt. Everest is actually measured from the sea level like all other mountains are. But in case of Mauna Loa, they measured it from its base. Cheers.

  6. Jon says:

    I read somewhere that a mountain the size of O. Mons couldn’t occur on Earth as the higher gravity would cause it to sink before it could reach anywhere near these heights. Very interesting though. Thanks.

  7. Michael says:

    There is a much more salient issue, unrelated to grammar. Mauana Loa is not the tallest mountain on earth from base to peak. That would be Mauna Kea, which is 10,203 meters tall.

  8. Scott says:

    Interesting. The three methods of measurement are Sea Level to Peak, Base to Peak, and Center of the (planet, asteroid, whatever) to Peak. I’m voting for Base to Peak as the new standard.

    The most commonly accepted, and unfair, method of measurement is from sea level, which is fine if the mountain in question is on a planet or body that HAS a sea. If not, then it wouldn’t even qualify to be considered.

    Center of Mass to Peak would be horribly unfair, as a one foot bump on Jupiter would still outshine Olympus Mons.

    Base to Peak removes the variables and allows each geologic feature to stand on it’s own (pun intended).

    Just my two cents worth.

  9. Bob says:

    Mona loa Is actually 10.41 miles high.

RSS feed for comments on this post. TrackBack URI

Leave a comment

Comments are moderated, and will not appear until Smithsonian.com has approved them. Smithsonian reserves the right not to post any comments that are unlawful, threatening, offensive, defamatory, invasive of a person's privacy, inappropriate, confidential or proprietary, political messages, product endorsements, or other content that might otherwise violate any laws or policies.

Spam protection by WP Captcha-Free

Advertisement



Follow Us

Travel with Smithsonian






Advertisement