Back to Search Start Over

NEAR at Eros: Imaging and Spectral Results

Authors :
Clark R. Chapman
Han Li
Mark S. Robinson
Donald K. Yeomans
Beth E. Clark
A. Harch
Paul G. Lucey
William J. Merline
Peter C. Thomas
James F. Bell
Deborah L. Domingue
R. L. Kirk
Christine Peterson
M. Bell
E. Hawkins
Michael C. Malin
Michael J. Gaffey
Dennis D. Wellnitz
Brian Carcich
Scott L. Murchie
David W. Dunham
Patrick H. Martin
Joseph Veverka
J. Joseph
Noam R. Izenberg
Louise M. Prockter
B. G. Williams
Robert W. Farquhar
J. K. Miller
Lucy A. McFadden
J. Warren
William M. Owen
Andrew F. Cheng
Source :
Science. 289:2088-2097
Publication Year :
2000
Publisher :
American Association for the Advancement of Science (AAAS), 2000.

Abstract

Eros is a very elongated (34 kilometers by 11 kilometers by 11 kilometers) asteroid, most of the surface of which is saturated with craters smaller than 1 kilometer in diameter. The largest crater is 5.5 kilometers across, but there is a 10-kilometer saddle-like depression with attributes of a large degraded crater. Surface lineations, both grooves and ridges, are prominent on Eros; some probably exploit planes of weakness produced by collisions on Eros and/or its parent body. Ejecta blocks (30 to 100 meters across) are abundant but not uniformly distributed over the surface. Albedo variations are restricted to the inner walls of certain craters and may be related to downslope movement of regolith. On scales of 200 meters to 1 kilometer, Eros is more bland in terms of color variations than Gaspra or Ida. Spectra (800 to 2500 nanometers) are consistent with an ordinary chondrite composition for which the measured mean density of 2.67 ± 0.1 grams per cubic centimeter implies internal porosities ranging from about 10 to 30 percent.

Details

ISSN :
10959203 and 00368075
Volume :
289
Database :
OpenAIRE
Journal :
Science
Accession number :
edsair.doi.dedup.....49bfcc5496a4695a3aa86c491b3ba2ea