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JP2 Vertices (126)

from PSP_003234_2210 (0,299m per pixel)

E03 Vertices (126)

PSP Vertices (126)

from PSP_003234_2210 (2,93m per pixel)

original (3)

Original Images

E03 #001

E03 #001 px= 161 py= -765

E03 #002

E03 #002 px= 287 py= -636

E03 #003

E03 #003 px= 369 py= -521

E03 #004

E03 #004 px= 799 py= -454

E03 #005

E03 #005 px= 1085 py= -448

E03 #006

E03 #006 px= 1486 py= -485

E03 #007

E03 #007 px= 1710 py= -439

E03 #008

E03 #008 px= 1793 py= -638

E03 #009

E03 #009 px= 1870 py= -868

E03 #010

E03 #010 px= 1845 py=-1072

E03 #011

E03 #011 px= 1901 py=-1552

E03 #012

E03 #012 px= 1797 py=-1848

E03 #013

E03 #013 px= 1627 py=-2125

E03 #014

E03 #014 px= 997 py=-2154

E03 #015

E03 #015 px= 159 py=-2174
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Wellcome!

We are pleased to welcome you on our homepage. Be informed on our online presence about research and results regarding the famous mountain on Mars in Cydonia Mensae region. As an oronym we continue to use the term 'Face of Mars', although the mesa only looked on the first fotos taken from it like face, lying half in shadow. These pictures are not a good example for pareidolia, the appearance of a face on the very first pictures is obvious. This does not apply for newer fotos, they do not show the appearance of a face. Only people who mean to identify a face on newer fotos may labour under pareidolia. But nevertheless the mesa has more properties, which are not usual for naturally formed mountains ...

Take a look around!                             Or ask a question: talk@mountains-on-mars-in-3d.net