Skip to content

All sites

Craters of the Moon National Monument

Unreviewed draft

This page was built from a teammate-supplied list. The text is teammate-written, unreviewed. Sources pending.

Summary

not provided

Location

Country
USA (Idaho)
Coordinates
43.42, -113.52
Elevation (m)
1800
Year first used as an analog
1969

Terrain and geology

not provided

Climate

not provided

Parameters matched

not provided

Why it is an analog

Mature NASA analog with flows, cones and lava tubes in one place.

Key differences: where the analogy breaks down

Basalt is K- and Fe-rich (not mare-like); seasonal snow and soil; vegetation.

Experiments done

Apollo 14 crew visited 1969; NASA SSERVI FINESSE team used it for lunar/Mars volcanic field science, LiDAR and handheld-instrument trials; lava-tube studies.

Experiments proposed

Lava-tube mapping for lunar skylight exploration; thermal-inertia measurements of flow textures; robotic cave mapping; EVA protocol testing.

How to adjust it

Restrict test zones to young flows; add simulant in tube floors; dark-adapted lighting inside tubes.

Access

not provided

Hazards

not provided

Sources

Sources pending (no sources in CSV).

v1 score, percentile and overlap flag

A descriptive lookup of scores v1 already stored. It is not a test, and a high percentile here does not show that this is a good analog.

v1 used this site
No. The nearest v1 site, "mdrs utah", is about 602.4 km away.

Stored v1 scores near Craters of the Moon National Monument
Score viewResultPercentileScoreDistance to tile (km)Overlap flag
Connecting Ridge C1, BaseScored53.40.12.9Not in a flagged tile
Connecting Ridge C1, Landing and mobilityScored57.20.12.9Not in a flagged tile
Connecting Ridge C1, Power and nightScored53.40.12.9Not in a flagged tile
Shackleton rim, BaseScored57.020.22.9Not in a flagged tile
Shackleton rim, Landing and mobilityScored62.523.12.9Not in a flagged tile
Shackleton rim, Power and nightScored57.014.72.9Not in a flagged tile

Overlap flag: whether the tile used for the score is one v1 flagged as stable in its top group across the Monte Carlo runs.

What these scores can and cannot tell you
  • This is a lookup of scores v1 already stored. It is descriptive and is not a test of the method.
  • A site is matched to the best-scoring tile that passed the gates within the match radius. A different radius would give different numbers.
  • Tiles are large compared with most sites, so a score describes the surrounding area, not the site itself.
  • Scores exist only for tiles that passed the land-cover and data gates. A gated-out or unscored site has no score, which says nothing about how good an analog it is.
  • Percentile is the share of scored tiles in that view with a lower score.
  • The Moon score is effectively terrain only. Mars is a low-confidence secondary result.
  • v1 failed its negative controls, so a high percentile here does not show that a site is a good analog.
  • The ranking is not checked against independent data. Gravity, air, dust and radiation are not scored.
  • Sites are compared with views of their own body only.
  • Match radius: 20 km, the radius v1 used.