{"id":6439,"date":"2013-06-21T14:39:30","date_gmt":"2013-06-21T21:39:30","guid":{"rendered":"http:\/\/planets.ucla.edu\/?p=6439"},"modified":"2021-01-18T01:36:33","modified_gmt":"2021-01-18T09:36:33","slug":"the-asteroid-vesta-in-the-light-of-dawn","status":"publish","type":"post","link":"http:\/\/planets.ucla.edu\/?p=6439","title":{"rendered":"The Asteroid Vesta in the Light of Dawn"},"content":{"rendered":"<figure id=\"attachment_6441\" aria-describedby=\"caption-attachment-6441\" style=\"width: 357px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/planets.ucla.edu\/wp-content\/uploads\/2013\/05\/Vesta.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\" wp-image-6441\" title=\"Vesta\" src=\"http:\/\/planets.ucla.edu\/wp-content\/uploads\/2013\/05\/Vesta.jpg\" alt=\"\" width=\"357\" height=\"357\" srcset=\"http:\/\/planets.ucla.edu\/wp-content\/uploads\/2013\/05\/Vesta.jpg 600w, http:\/\/planets.ucla.edu\/wp-content\/uploads\/2013\/05\/Vesta-150x150.jpg 150w, http:\/\/planets.ucla.edu\/wp-content\/uploads\/2013\/05\/Vesta-300x300.jpg 300w\" sizes=\"auto, (max-width: 357px) 100vw, 357px\" \/><\/a><figcaption id=\"caption-attachment-6441\" class=\"wp-caption-text\">An image obtained of the asteroid Vesta from NASA\u2019s Dawn spacecraft from a distance of 3,200 miles. Image Credit: NASA\/JPL-Caltech\/UCLA\/MPS\/DLR\/IDA<\/figcaption><\/figure>\n<p>On September 27th, 2007, NASA\u2019s Dawn spacecraft left Earth and began a multi-year journey to two of the largest objects in the solar system\u2019s main asteroid belt.\u00a0 The first stop on its interplanetary roadtrip was the asteroid Vesta.\u00a0 Dawn reached the Arizona-sized chunk of primordial rock in 2011, providing scientists with the first close-up view of the asteroid\u2019s ancient surface.<\/p>\n<p>A leftover remnant from the formation of the solar system over four billion years ago, Vesta may be similar in composition to the larger bits of celestial debris that originally came together to form the inner planets.\u00a0 Scientists studying our planet\u2019s origins hope that Vesta will reveal clues about our past that have long been erased by plate tectonics and weathering on Earth.<\/p>\n<p>\u201cStudying Vesta is like going back to the beginning of the solar system,\u201d said Jennifer Scully, a third-year UCLA graduate student working on the Dawn mission. \u201cIt is kind of like a fossil of the sort of bodies that were around that combined to make the Earth,\u201d she said.\u00a0 Scully, the lead mapper for two large areas on Vesta, makes geological maps of the asteroid\u2019s surface in order to interpret the history of different features and formations.<\/p>\n<p>What she has found so far has been surprising.\u00a0 \u201cWe discovered a lot of things that were unexpected at Vesta,\u201d she said.\u00a0 Grayscale and color images taken by Dawn\u2019s framing camera show a remarkable range of shades on the surface of Vesta, featuring both very bright and very dark material. \u201cIt\u2019s very colorful,\u201d said Scully.\u00a0 \u201cWe think the dark material is residue from meteorites called carbonaceous chondrites that have hit the surface.\u201d<\/p>\n<p>Data from Dawn\u2019s instruments including the camera\u2019s seven color filters, a spectrometer, and a neutron detector help scientists characterize surface deposits and divide Vesta into areas depending on age, composition, and morphology.\u00a0 But sometimes this close-up view of Vesta raises more questions than answers.<\/p>\n<p>\u201cWe found both straight and sinuous gully features and I\u2019m investigating what sort of flow(s) formed them,\u201d said Scully. Whether or not some of the gully features could have been carved by molten rock is under investigation.\u00a0 \u201cThe team has not found any definitive features of volcanism,\u201d Scully said.\u00a0 \u201cThere could have been activity early on, but the evidence has been wiped clean by billions of years of impacts.\u201d<\/p>\n<p>Evidence of many of these impacts is preserved on Vesta\u2019s surface in the form of craters. These craters range in size from being so small that Dawn\u2019s camera can barely resolve them to being so large that they have diameters nearly as big as Vesta. The two largest impact basins on the asteroid, named Veneneia and Rheasilvia, are found in Vesta\u2019s southern hemisphere. Scully is one of many Dawn scientists who are working to connect these impact basins with structures in Vesta\u2019s northern hemisphere. \u201cThe current understanding is that each of these large impacts sent shock waves through Vesta, which formed large-scale ridges and depressions on the opposite side,\u201d said Scully.<\/p>\n<p>The Dawn spacecraft does not only examine the surface of an asteroid, it can also give scientists clues about its internal structure.\u00a0 \u201cFrom the way the gravity pulls on the spacecraft you can tell about the internal layers and the size of the core,\u201d said Scully.\u00a0 From examining how Vesta\u2019s gravitational field tugs on Dawn, scientists believe that Vesta has a distinct crust, mantle, and core like Earth.<\/p>\n<p>The same is likely not true for the asteroid Ceres, Vesta\u2019s younger cousin and the next and final stop for the Dawn spacecraft.\u00a0 After remaining in orbit around Vesta for one year, the Dawn spacecraft took its leave in September of 2012 to begin a three-year journey to Texas-sized Ceres, the largest object in the main asteroid belt located between Mars and Jupiter.\u00a0 Unlike Vesta, scientists think Ceres may harbor large amounts of water ice under its surface.\u00a0 Because Ceres is wetter than Vesta, it will present a whole new set of questions.\u00a0 Scully looks forward to directly comparing the data collected from the two asteroids when the spacecraft arrives at Ceres in 2015.<\/p>\n<p>For Scully, the decision to come to UCLA and work with Professor Christopher Russell was a \u201cno brainer.\u201d\u00a0 \u201cGetting to work on an actual active mission is pretty awesome.\u00a0 You get to meet a lot of people and really see how a team works,\u201d she said.\u00a0 In addition to her work on the geology of Vesta, Scully helped create an online system called Asteroid Mappers where citizen scientists can identify features on Vesta using real data collected by Dawn.<\/p>\n<p>Watch a video profile of Jennifer Scully <a href=\"http:\/\/www.youtube.com\/watch?feature=player_embedded&amp;v=KkM4iLSGXm4\">here<\/a>.\u00a0 Learn more about her research <a href=\"http:\/\/www.youtube.com\/watch?feature=player_embedded&amp;v=iFzJJ6BXE2Q\">here<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>On September 27th, 2007, NASA\u2019s Dawn spacecraft left Earth and began a multi-year journey to two of the largest objects in the solar system\u2019s main asteroid belt.\u00a0 The first stop on its interplanetary roadtrip was the asteroid Vesta.\u00a0 Dawn reached the Arizona-sized chunk of primordial rock in 2011, providing scientists with the first close-up view &hellip; <\/p>\n<p class=\"link-more\"><a href=\"http:\/\/planets.ucla.edu\/?p=6439\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;The Asteroid Vesta in the Light of Dawn&#8221;<\/span><\/a><\/p>\n","protected":false},"author":9,"featured_media":3136,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[296,32],"tags":[323,324,322],"class_list":["post-6439","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-featured","category-news","tag-dawn","tag-jennifer-scully","tag-vesta"],"_links":{"self":[{"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/posts\/6439","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/users\/9"}],"replies":[{"embeddable":true,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=6439"}],"version-history":[{"count":9,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/posts\/6439\/revisions"}],"predecessor-version":[{"id":11318,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/posts\/6439\/revisions\/11318"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=\/wp\/v2\/media\/3136"}],"wp:attachment":[{"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=6439"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=6439"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/planets.ucla.edu\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=6439"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}