From fifty kilometers above asteroid Eros, the surface inside one of its largest craters appears covered with an unusual substance: regolith [
http://science.canb
]. The thickness and composition of the surface dust that is regolith [
http://adsabs.harva
] remains a topic of much research. Much of the regolith on 433 Eros [
http://near.jhuapl.
] was probably created by numerous small impacts during its long history. In this representative-color view [
http://near.jhuapl.
] taken by the robot spacecraft NEAR-SHOEMAKER [
http://near.jhuapl.
] that orbited Eros [
http://near.jhuapl.
] in 2000 and 2001, brown areas indicate regolith [
http://near.jhuapl.
] that has been chemically altered by exposure to the solar wind [
http://antwrp.gsfc.
] during micrometeorite [
http://www.solarvie
] impacts. White areas are thought to have undergone relatively less exposure. The boulders visible [
http://antwrp.gsfc.
] inside the crater appear brown, indicating either that they are old enough to have a surface itself tanned by the solar wind [
http://www-istp.gsf
], or that they have somehow become covered with some dark surface regolith [
http://antwrp.gsfc.
].
Explanation
From fifty kilometers above asteroid Eros, the surface inside one of its largest craters appears covered with an unusual substance: regolith [
http://science.canb
]. The thickness and composition of the surface dust that is regolith [
http://adsabs.harva
] remains a topic of much research. Much of the regolith on 433 Eros [
http://near.jhuapl.
] was probably created by numerous small impacts during its long history. In this representative-color view [
http://near.jhuapl.
] taken by the robot spacecraft NEAR-SHOEMAKER [
http://near.jhuapl.
] that orbited Eros [
http://near.jhuapl.
] in 2000 and 2001, brown areas indicate regolith [
http://near.jhuapl.
] that has been chemically altered by exposure to the solar wind [
http://antwrp.gsfc.
] during micrometeorite [
http://www.solarvie
] impacts. White areas are thought to have undergone relatively less exposure. The boulders visible [
http://antwrp.gsfc.
] inside the crater appear brown, indicating either that they are old enough to have a surface itself tanned by the solar wind [
http://www-istp.gsf
], or that they have somehow become covered with some dark surface regolith [
http://antwrp.gsfc.
].
Explanation