New Enceladus Maps

Enceladus South Polar Map Full-Res: PIA12566

The northern and southern hemispheres of Enceladus are seen in these polar stereographic maps, mosaicked from the best-available Cassini and Voyager clear-filter images. Each map is centered on one of the poles and surface coverage extends to the equator. Grid lines show latitude and longitude in 30-degree increments. The scale in the full-size versions of these maps is 110 meters (360 feet) per pixel.

Enceladus South Polar Map Full-Res: PIA12566

The northern and southern hemispheres of Enceladus are seen in these polar stereographic maps, mosaicked from the best-available Cassini and Voyager clear-filter images. Each map is centered on one of the poles and surface coverage extends to the equator. Grid lines show latitude and longitude in 30-degree increments. The scale in the full-size versions of these maps is 110 meters (360 feet) per pixel. These maps are updated versions of those released in October 2009 (see Enceladus Polar Maps – North Pole – October 2009 and Enceladus Polar Maps – South Pole – October 2009 ).

These two maps show that the character of terrains near the north pole differs strongly from those near the south pole. Terrain near the north pole is among the most heavily cratered and oldest on the surface of Enceladus. The northern hemisphere map shows that a broad band of cratered terrain extends from the equator on the Saturn-facing side (centered on 0 degrees longitude), over the pole and to the equator on the anti-Saturn side (centered on 180 degrees longitude). Terrains near the equator and mid-latitudes on the leading (90 degrees west longitude) and trailing (270 degrees west longitude) sides of Enceladus are much less heavily cratered and are characterized by intense zones of fracturing and faulting.

As seen in the southern hemisphere map, the band of cratered terrain at 0 and 180 degrees longitude extends southward from the equator. However, poleward of about 55 degrees south latitude, the cratered terrain is interrupted and replaced by a conspicuously fractured circumpolar terrain that is nearly devoid of impact craters. In contrast to the very old north polar terrains, the south circumpolar terrains are among the youngest on the surface of Enceladus.

Within the south circumpolar region is a group of prominent parallel “stripes” made up of fractures that are delineated by relatively dark albedo markings flanking the sides of each fracture.
An interesting property of the parallel fracture system is that each appears to turn back at its westernmost segment as if it has been “bent” or “folded” into a hook-like curve. Similar patterns of folded or kinked fractures can be found throughout the region — a unique feature of the south polar terrain.

Enceladus North Polar Map Full-Res: PIA12565

Map of Enceladus Full-Res: PIA12564

This mosaic shows an updated global map of Saturn’s icy moon Enceladus, created using images taken during Cassini spacecraft flybys. The map incorporates new images taken during flybys in October and November 2009.

This map is an update to the version released in October 2009 (see PIA11680). Like other recent Enceladus global maps, this mosaic was shifted by 3.5 degrees to the west, compared to 2006 versions, to be consistent with the International Astronomical Union longitude definition for Enceladus.
The so-called “tiger stripe” features that have captivated Cassini scientists can be seen distorted by the projection method in the lower middle left and lower middle right of the image.
This map contains just one image from NASA’s Voyager 2 spacecraft, which visited Enceladus more than 25 years ago. That image fills in the top left of the map from 90 degrees north down to as low as 50 degrees north in places. Other parts of the map include low-resolution Cassini Imaging Science Subsystem images.

The map is an equidistant (simple cylindrical) projection and has a scale of 110 meters (360 feet) per pixel at the equator. The mean radius of Enceladus used for projection of this map is 252 kilometers (157 miles).

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington, D.C.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington, D.C. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The imaging operations center is based at the Space Science Institute in Boulder, Colo.

For more information about the Cassini-Huygens mission visit http://saturn.jpl.nasa.gov . The Cassini imaging team homepage is at http://ciclops.org . Credit: NASA/JPL/Space Science Institute