Difference between revisions of "Smith and Sanchez, 1973"

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<div style="margin-left: 1em">[#toc0 ]</div><div style="margin-left: 2em">[#x-Description Description]</div><div style="margin-left: 2em">[#x-Additional Information Additional Information]</div><div style="margin-left: 2em">[#x-LPOD Articles LPOD Articles]</div><div style="margin-left: 2em">[#x-Bibliography Bibliography]</div></div><br />  
 
<div style="margin-left: 1em">[#toc0 ]</div><div style="margin-left: 2em">[#x-Description Description]</div><div style="margin-left: 2em">[#x-Additional Information Additional Information]</div><div style="margin-left: 2em">[#x-LPOD Articles LPOD Articles]</div><div style="margin-left: 2em">[#x-Bibliography Bibliography]</div></div><br />  
 
==Description==
 
==Description==
  Gene Smith and Anthony Sanchez defined a '''Morphology Index''' (MI) based upon a numeric classification of crater walls, central peaks and floors. This is functionally equivalent to classifying craters into the types defined by [/Wood%20and%20Anderson%2C%201982 Wood and Anderson, 1982]. MI increases with crater diameter as craters change from simple to complex shapes.<br />  MI and its components are given in the Moon WIki for the few hundred craters cataloged by Smith and Snachez and '''Smith and Hartnell (1978)'''<br /> <br />  
+
  Gene Smith and Anthony Sanchez defined a '''Morphology Index''' (MI) based upon a numeric classification of crater walls, central peaks and floors. This is functionally equivalent to classifying craters into the types defined by [[Wood%20and%20Anderson%2C%201982|Wood and Anderson, 1982]]. MI increases with crater diameter as craters change from simple to complex shapes.<br />  MI and its components are given in the Moon WIki for the few hundred craters cataloged by Smith and Snachez and '''Smith and Hartnell (1978)'''<br /> <br />  
 
==Additional Information==
 
==Additional Information==
 
  MI is the addition of scores for TSI + FI + CPI.<br />  TSI - Terrace-Shape Index - the form of crater terraces/slumps and the crater floor diameter / crater diameter (CFD/CD).<br />  FI - Floor Index - floor texturing.<br />  CPI - Central Peak Index - morphology and number of central peaks.<br />  This table shows the scoring for each index.<br /> [[Image:Smith%26Sanchez1973-MI.jpg|Smith&Sanchez1973-MI.jpg]]<br /> <br />  
 
  MI is the addition of scores for TSI + FI + CPI.<br />  TSI - Terrace-Shape Index - the form of crater terraces/slumps and the crater floor diameter / crater diameter (CFD/CD).<br />  FI - Floor Index - floor texturing.<br />  CPI - Central Peak Index - morphology and number of central peaks.<br />  This table shows the scoring for each index.<br /> [[Image:Smith%26Sanchez1973-MI.jpg|Smith&Sanchez1973-MI.jpg]]<br /> <br />  

Revision as of 16:17, 15 April 2018

18

(glossary entry)

Table of Contents

[#toc0 ]
[#x-Description Description]
[#x-Additional Information Additional Information]
[#x-LPOD Articles LPOD Articles]
[#x-Bibliography Bibliography]

Description

Gene Smith and Anthony Sanchez defined a Morphology Index (MI) based upon a numeric classification of crater walls, central peaks and floors. This is functionally equivalent to classifying craters into the types defined by Wood and Anderson, 1982. MI increases with crater diameter as craters change from simple to complex shapes.
MI and its components are given in the Moon WIki for the few hundred craters cataloged by Smith and Snachez and Smith and Hartnell (1978)

Additional Information

MI is the addition of scores for TSI + FI + CPI.
TSI - Terrace-Shape Index - the form of crater terraces/slumps and the crater floor diameter / crater diameter (CFD/CD).
FI - Floor Index - floor texturing.
CPI - Central Peak Index - morphology and number of central peaks.
This table shows the scoring for each index.
Smith&Sanchez1973-MI.jpg

LPOD Articles


Bibliography

Smith, EI and AG Sanchez (1973) Fresh lunar craters: Morphology as a function of diameter, a possible criterion for crater origin. Modern Geology, 4, 51-59.
Smith, EI and JA Hartnell (1978) Crater size-shape profiles for the moon and mercury: Terrain effects and interplanetary comparisons. Earth, Moon, and Planets, 19, # 4, 479-511. Abstract


This page has been edited 1 times. The last modification was made by - tychocrater tychocrater on Jun 13, 2009 3:24 pm - mgx2