Title: MSL landing sites in ancient layered terrain: Becquerel Crater
1MSL landing sites in ancient layered terrain
Becquerel Crater
John Bridges1 and Matt Balme2
1Planetary Space Sciences Research Institute,
Open University, UK 2Dept. of Earth Sciences,
Open University, UK and Planetary Science
Institute, Tucson, Az.
2Assess Past Habitability through Rover Traverse
over Interior Layered Deposits (ILD)
- Traverse over ILD would allow sedimentary log
over millions years of depositional history - Best way of achieving MSL aims?
- Impact, lacustrine, fluvial hypotheses assessed
with extensive outcrop
0.2 km
M1201064 352.25oE, 21.35oN (east side of ILD)
3Aim Land beside ILD and traverse to their margin
and onto them
ILD
ILD
MOLA shaded terrain map 20 km landing ellipses
for consideration
Bridges
Balme
Becquerel
Bridges
Balme
Becquerel
4Becquerel Crater
- 167 km diameter crater in Arabia Terra 22oN,
352oE - Contains 900 km2 exposure of Noachian Interior
Layered Deposits (ILD) - -2.6 to -3.8 km elevation
- gt300 TI units (dust conditions not prohibitive),
rock abundance 4-12 - No substantial current ground-ice detected by
Gamma-Ray spectrometer so satisfies planetary
protection constraint
ILD
20 km
5Becquerel Crater
167 km diameter crater in Arabia
Terra 22
o
N, 352
o
E
Contains 900 km
2
exposure of
Noachian Interior Layered
Deposits (ILD)
-
2.6 to
-
3.8 km elevation
gt300 TI units (dust conditions
not prohibitive), rock abundance
4
-
12
No substantial current ground
-
ice
ILD
detected by Gamma
-
Ray
spectrometer so satisfies
planetary protection constraint
MOLA 128 ppd gridded data
Bridges
Balme
Becquerel
Bridges
Balme
Becquerel
6Becquerel Crater
167 km diameter crater in Arabia
Terra 22
o
N, 352
o
E
2
Contains 900 km
exposure of
Noachian Interior Layered
Deposits (ILD)
-
2.6 to
-
3.8 km elevation
gt300 TI units (dust conditions
not prohibitive), rock abundance
4
-
12
ILD
ILD
No substantial ground
-
ice
detected by Gamma
-
Ray
spectrometer so satisfies
planetary protection constraint
20 km
THEMIS night
7Are These Deposits Accessible?
8- Two proposed 20 km landing ellipses to east A
and west B of ILD - 351.386E, 21.478N (centre A)
- 352.522E, 21.320N (centre B)
A
B
ILD
THEMIS daylight
20 km
9- Two proposed 20 km landing ellipses to east A
and west B of ILD - 351.386E, 21.478N (centre A)
- 352.522E, 21.320N (centre B)
A
B
ILD
10 km
MOC na mosaic
10Roughness and Aeolian Deposits
- Green is dark dunes/sheets
- Around margins of ILD, dark sand
- is in sheets rather than barchans
ILD
10 km
11Ellipse A Roughness
2.5 km
- THEMIS vis. Yellow is rough area (15 of
ellipse)
12Ellipse A
ILD
0.2 km
- THEMIS NIGHT IR
- surface temperature 180-200K
- THEMIS V09899025
- Dark barchans
13Ellipse A
M0701459
E0502646
0.25 km
- Typical terrain relatively rough with aeolian
deposits
14Ellipse B
2
1
2.5 km
- THEMIS IR night
- 175 (dark)-200K (light)
15Ellipse B
Area 1
Area 2
2.5 km
- Polygonal terrain past ice terrain ? (but
little or no current ice) - Less rough than ellipse A
16Elevation
MOLA shaded map
- A and B ellipses -3.6 to -3.8 km,
- ILD -3.1 to -3.7 km
17Slopes and ILD Access
- Most slopes in A and B lt5o
- Slopes between ellipses and
- ILD 2 10o
- Base cliffs and top surface of
- ILD could be accessed by rover
A
B
ILD
18Summary Becquerel can reveal past Martian
Environment
- 352.522E, 21.320N (centre B safer ellipse)
- Slopes, terrain allow landing and access to
margin and probably onto ILD - Satisfies planetary protection
- Accessing ILD allows best analysis
- of past martian habitability over millions of
years
Interior Layered Deposits
e0200375 (21.6oN, 351.6oE). Width 1.5 km, 3m/px
19Summary Becquerel can reveal past Martian
Environment
- 352.522E, 21.320N (centre B safer ellipse)
- Slopes, terrain allow landing and access to
margin and probably onto ILD - Satisfies planetary protection
- Accessing ILD allows best analysis
- of past martian habitability over millions of
years - Issues some dark aeolian
- deposits and some rough terrain
- in margin of ellipse B
Interior Layered Deposits
e0200375 (21.6oN, 351.6oE). Width 1.5 km, 3m/px