Why exactly is the feature on Io called a volcano, and the feature on Enceladus called a geyser? Color coding in this map of a far-northern site on Mars indicates the change in nighttime ground-surface temperature between summer and fall. Neither is the case on earth: The plate moves away from the hot spot, transporting built up rocks with it and causing the magma to find another outlet a few miles over. As a result, they crust on Mars can support mountains that the plates on Earth could not. Candidates scoring 100% in very small polling stations — violation of secret ballot? NASA Science Mars Exploration Program. Hawaii also tends to be a place where you can see water erosion happen in a pretty spectacular way. Mt. A leading-edge research firm focused on digital transformation. This image captured by NASA's 2001 Mars Odyssey spacecraft shows 'streamers' of clouds created by katabatic winds at the north polar cap. The Thermal Emission Imaging System (THEMIS) was developed by Arizona State University, Tempe, in collaboration with Raytheon Santa Barbara Remote Sensing. rev 2020.11.4.37952, Sorry, we no longer support Internet Explorer, The best answers are voted up and rise to the top, Earth Science Stack Exchange works best with JavaScript enabled, Start here for a quick overview of the site, Detailed answers to any questions you might have, Discuss the workings and policies of this site, Learn more about Stack Overflow the company, Learn more about hiring developers or posting ads with us, if your volcano mauna loa 10km high were, it would be higher then mont everest. Orbit Number: 77209 Latitude: 17.991 Longitude: 225.786 Instrument: VIS Captured: 2019-05-11 16:44. Well... not really.

It's a bit like when you step onto an ice flow: it just sinks down a bit. It's also pretty fair when you are considering the whole solar system, since sea level is very different, or missing entirely, on other planets, through no fault of the volcano, @AsteroidsWithWings the volcano knows what it did. This process is called "isostatic adjustment", and you can think of it as the plate just sinking down into the region below that consists of a (somewhat) liquid state of rock which just moves to the side. Massif Central, although smaller, is definitely not ridiculous compared to Olympus Mons. Fans and ribbons of dark sand dunes creep across the floor of Bunge Crater in response to winds blowing from the direction at the top of the picture. This ridge is estimated to be 6 miles high — higher than the tallest point on Mt. A small section of Dao Vallis in shown in this VIS image. NASA/MOLA Science Team/ O. de Goursac, Adrian Lark Why is Massanutten mountain so dramatically different than surrounding mountains?