Skip to main content Accessibility help
×
Hostname: page-component-8448b6f56d-qsmjn Total loading time: 0 Render date: 2024-04-23T14:52:18.885Z Has data issue: false hasContentIssue false

Oxia Palus (MC-11)

from Map Sheets

Published online by Cambridge University Press:  16 August 2019

Kenneth S. Coles
Affiliation:
Indiana University of Pennsylvania
Kenneth L. Tanaka
Affiliation:
United States Geological Survey, Arizona
Philip R. Christensen
Affiliation:
Arizona State University
Get access

Summary

The Oxia Palus quadrangle is dominated in the east by the mid-elevation Arabia Terra (1,500–3,500 m below datum), with ancient cratered terrain transitioning from the southern highlands down to the northern plains. Arabia Terra includes a portion of Meridiani Planum, north of the Mars Exploration Rover-B (Opportunity) landing site (MC-19). Mawrth Vallis is the only large valley coming from this portion of Arabia Terra that has a mouth opening directly into the northern plains across the dichotomy boundary. The western half of the quadrangle includes portions of Margaritifer Terra and Xanthe Terra highland terrains, which are dissected by enormous outflow channels. These formed by catastrophic floods that left behind grooved channels, streamlined islands, chaotic terrain, braided-channel patterns, and the southern margin of the smooth northern plains deposits. From east to west, Ares, Tiu, Simud, and Shalbatana Valles carve curvilinear paths through the highland terrain until merging at the southern margins of Chryse Planitia. Chryse, at 3,000–4,000 m below datum, dominates the northwest portion of the quadrangle and lies within an ~1,600-km-diameter, ancient, largely degraded, and buried impact basin. The Mars Pathfinder landing site, which included the first rover (named Sojourner) to navigate on Mars, is located in Tiu Valles near the edge of the Ares Vallis deposits.

Type
Chapter
Information
The Atlas of Mars
Mapping its Geography and Geology
, pp. 126 - 131
Publisher: Cambridge University Press
Print publication year: 2019

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×