{"id":1912,"date":"2006-02-12T10:30:00","date_gmt":"2006-02-12T15:30:00","guid":{"rendered":""},"modified":"2006-02-12T10:30:00","modified_gmt":"2006-02-12T15:30:00","slug":"cassini-images-reval-active-moon","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=1912","title":{"rendered":"Cassini Images Reval Active Moon"},"content":{"rendered":"<p>Jets of fine, icy particles streaming from Saturn&#8217;s moon Enceladus were captured in recent images from NASA&#8217;s Cassini spacecraft. The images provide unambiguous visual evidence the moon is geologically active. <\/p>\n<p>&#8220;For planetary explorers like us, there is little that can compare to the sighting of activity on another solar system body,&#8221; said Dr. Carolyn Porco, Cassini imaging team leader at the Space Science Institute in Boulder, Colo. &#8220;This has been a heart-stopper, and surely one of our most thrilling results.&#8221; <\/p>\n<p>The Cassini images clearly show multiple jets emanating from the moon&#8217;s south polar region. Based on earlier data, scientists strongly suspected these jets arise from warm fractures in the region. The fractures, informally dubbed &#8220;tiger stripes,&#8221; are viewed essentially broadside in the new images.<br \/>\n<!--more--><br \/>\nThe fainter, extended plume stretches at least 300 miles above the surface of Enceladus, which is only 300 miles wide. Cassini flew through the plume in July, when it passed a few hundred kilometers above the moon. During that flyby, Cassini&#8217;s instruments measured the plume&#8217;s constituent water vapor and icy particles. <\/p>\n<p>Imaging team members analyzed images of Enceladus taken earlier this year at similar viewing angles. It was a rigorous effort to demonstrate earlier apparitions of the plumes, seen as far back as January, were in fact real and not due to imperfections in the camera. <\/p>\n<p>The recent images were part of a sequence planned to confirm the presence of the plumes and examine them in finer detail. Imaging team member Dr. Andrew Ingersoll from the California Institute of Technology in Pasadena, said, &#8220;I think what we&#8217;re seeing are ice particles in jets of water vapor that emanate from pressurized vents. To form the particles and carry them aloft, the vapor must have a certain density, and that implies surprisingly warm temperatures for a cold body like Enceladus.&#8221; <\/p>\n<p>Imaging scientists are comparing the new images to earlier Cassini data in hopes of arriving at a more detailed, three-dimensional picture of the plumes and understanding how activity has come about on such a small moon. They are not sure about the precise cause of the moon&#8217;s unexpected geologic vitality. <\/p>\n<p>&#8220;In some ways, Enceladus resembles a huge comet,&#8221; said Dr. Torrence Johnson, imaging team member from NASA&#8217;s Jet Propulsion Laboratory (JPL) in Pasadena. &#8220;Only, in the case of Enceladus, the energy source for the geyser-like activity is believed to be due to internal heating by perhaps radioactivity and tides rather than the sunlight which causes cometary jets.&#8221; The new data also give yet another indication of how Enceladus keeps supplying material to Saturn&#8217;s gossamer E ring. <\/p>\n<p>The Cassini-Huygens mission is a cooperative project of NASA, the European and Italian Space Agencies. JPL, a division of the Caltech, manages the mission for NASA&#8217;s Science Mission Directorate. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The imaging team is based at the Space Science Institute. <\/p>\n<p>For the latest Cassini images on the Web, including a time sequence showing the plumes, visit: <br \/>\n<a href=\"http:\/\/saturn.jpl.nasa.gov \"   target=\"_blank\"  ><br \/>\nhttp:\/\/saturn.jpl.nasa.gov  <\/a> <\/p>\n","protected":false},"excerpt":{"rendered":"<p>Jets of fine, icy particles streaming from Saturn&#8217;s moon Enceladus were captured in recent images from NASA&#8217;s Cassini spacecraft. The images provide unambiguous visual evidence the moon is geologically active.&hellip; <\/p>\n","protected":false},"author":1,"featured_media":612598,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[4],"tags":[],"class_list":["post-1912","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-NASA"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/1912","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1912"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/1912\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/612598"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1912"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=1912"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=1912"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}