LUNAR RIVERS

被引:49
作者
LINGENFELTER, RE
PEALE, SJ
SCHUBERT, G
机构
[1] Institute of Geophysics, Department of Planetary and Space Science, University of California
关键词
D O I
10.1126/science.161.3838.266
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Mature meanders in lunar sinuous rills strongly suggests that the rills are features of surface erosion by water. Such erosion could occur under a pressurizing ice cover in the absence of a lunar atmosphere. Water, outgassed from the lunar interior and trapped beneath a layer of permafrost, could be released by a meteoritic impact and overflow the crater to form an ice-covered river. A sinuous rill could be eroded in about 100 years.
引用
收藏
页码:266 / +
页数:1
相关论文
共 18 条
[1]   INTERPRETATION OF SCHROTERS VALLEY + OTHER LUNAR SINUOUS RILLS [J].
CAMERON, WS .
JOURNAL OF GEOPHYSICAL RESEARCH, 1964, 69 (12) :2423-+
[2]   DENSITY OF LUNAR SURFACE [J].
CAMPBELL, MJ ;
ULRICHS, J ;
GOLD, T .
SCIENCE, 1968, 159 (3818) :973-&
[3]  
CHRISTENSEN EM, 1967, JPL321177 TECH REP 2, P111
[4]  
GOLD T, 1961, J GEOPHYS RES, V66, P2531
[5]  
GOLD T, 1966, NATURE LUNAR SURFACE, P107
[6]  
Gold T., 1964, ORIGIN EVOLUTION ATM, P249
[7]   ON PARTICLE SIZE DISTRIBUTION OF LUNAR SOIL [J].
HAPKE, BW .
PLANETARY AND SPACE SCIENCE, 1968, 16 (01) :101-&
[8]   SURFACE STRUCTURE AND MECHANICAL PROPERTIES OF LUNAR MARIA [J].
JAFFE, LD .
JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (06) :1727-&
[9]  
KUIPER GP, 1966, JPL32800 TECH REP 2, P35
[10]  
NEVILL E, MOON CONDITION CONFI, P72