Previous Page  19 / 52 Next Page
Information
Show Menu
Previous Page 19 / 52 Next Page
Page Background

SEPTEMBER-OCTOBER 2017

SPACE CHRONICLES

ice that subsequently inter-

acted with the ancient, vol-

canic mountain rocks.

Numerous craters in vari-

ous states of degradation

pockmark the entire scene,

testament to the region’s

long history. Perhaps the

most noticeable craters are

the two situated side by

side close to the centre of

the scene (below), their

breached crater walls con-

necting them and giving the appear-

ance of a figure of eight shape.

Another interesting crater lies to the

left, nestled into the side of a hum-

wider crater, punching through to

deeper layers below. The rich diver-

sity of geologic features in this re-

gion – and in this image alone –

showcases the dynamic environment

the planet has witnessed through

time, evolving from a warmer wetter

climate that enabled liquid water to

flow freely across the surface, to the

arid world that we see today.

T

his map shows the lo-

cation of Libya Montes

in context of the sur-

rounding region. The re-

gion outlined by the larger

white box indicates the

area imaged during Mars

Express orbit 16647 on 21

February 2017. The small

box in the centre high-

lights the focus of the as-

sociated image release. In

this context image, north

is up. [NASA MGS MOLA

Science Team]

T

he colour-coded topographic view shows relative heights and depths of ter-

rain in the Libya Montes region on Mars. As indicated in the key at top right,

whites and reds represent the highest terrain, while blue/purple is the lowest.

The color-coded topographic view is based on a digital terrain model of the re-

gion, from which the topography of the landscape can be derived. [ESA/DLR/FU

Berlin, CC BY-SA 3.0 IGO]

mocky mountain. Inevitably, its rim

collapsed onto the valley floor be-

neath. Further left again, and a small

crater has imprinted into the larger,

!