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Myvatn and Krafla lava fields

Unreviewed draft

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

Summary

not provided

Location

Country
Iceland
Coordinates
65.65, -16.80
Elevation (m)
400
Year first used as an analog
1965

Terrain and geology

not provided

Climate

not provided

Parameters matched

not provided

Why it is an analog

Apollo training on young basaltic fissure flows.

Key differences: where the analogy breaks down

Lakes and vegetation; rootless cones require water (not lunar).

Experiments done

Apollo crews trained here in 1965 and 1967 on fissure-fed basalt, spatter ramparts and rootless cones; later volcanology of the Krafla Fires (1724-29, 1975-84) eruptions used to interpret lunar rilles and fissures.

Experiments proposed

Fresh-lava traverses; geothermal-powered habitat concepts; fissure and graben mapping.

How to adjust it

Restrict tests to the 1975-84 Krafla flows (bare); overlay basaltic simulant lanes; use geothermal heat to run thermal-cycling tests alongside cold ground.

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
Unknown. The nearest v1 site, "askja", is about 69.0 km away, and the files cannot say whether v1 meant the same place.

Stored v1 scores near Myvatn and Krafla lava fields
Score viewResultPercentileScoreDistance to tile (km)Overlap flag
Connecting Ridge C1, BaseScored89.715.516.3Not in a flagged tile
Connecting Ridge C1, Landing and mobilityScored95.517.716.3Not in a flagged tile
Connecting Ridge C1, Power and nightScored89.711.316.3Not in a flagged tile
Shackleton rim, BaseScored90.836.84.0Not in a flagged tile
Shackleton rim, Landing and mobilityScored98.442.14.0In a flagged tile
Shackleton rim, Power and nightScored90.826.74.0Not 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.