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Phobos · Crater · 5th largest named feature

Hall

Asaph; American astronomer, discoverer of Phobos and Deimos (1829-1907).

What Hall is

Hall is a crater — a circular depression, almost always an impact scar — on Phobos, 5.4 km across, centred at 80.0° S, 150.0° E. It is the 5th largest named feature on Phobos and the 3rd largest of its class there.

Where the name comes from

Asaph; American astronomer, discoverer of Phobos and Deimos (1829-1907). The International Astronomical Union approved the name in 1973, under the theme it applies to every crater on Phobos. Of the 17 features of this class catalogued on Phobos, the naming categories run Ireland (8), American (5), France (1), Germany (1).

Feature class
a circular depression, almost always an impact scar
Diameter
5.4 km
about a 5 km run
Coordinates
80.0° S, 150.0° E
Planetocentric, on Phobos
Name approved
1973
By the IAU Working Group for Planetary System Nomenclature
Naming category
American
North America

What it would take to settle Hall

Phobos scores 48.7 as a world. That number is the same for every square metre of it — but sunlight, water, radiation and the ground under your feet are not. This is the same question asked at 80.0° S, 150.0° E.

Settlement difficulty here
54.5/ 100
Harder than most of this world
Phobos overall
48.7
5.8 harder than the median site
Ranked
19th
of 20 named places on Phobos

What this spot has going for it is ground mixed ground — a rim, a floor and slopes between them. What works against it is sunlight 17% of the sunlight the sunniest latitude on Phobos gets.

Computed from Hall's catalogued latitude, longitude and feature class — 68% of the model's weight had a basis here, and 3 axes were dropped as not applicable to Phobos (radiation geometry, earth link, known ground). Gravity, pressure, delta-v and distance from the Sun are the same everywhere on Phobos and are already counted in the world's own index, not again here.

What this cannot see: elevation. Slope, local shadowing and the polar “peaks of eternal light” — ridge tops near the poles of a barely tilted world that catch sun almost continuously while a crater floor kilometres away never does — need a terrain model this does not have. Where a real mission targets a pole, that is usually why.

What is next to it

The largest crater features on Phobos

All 17 craters on Phobos — mapped together, with the naming theme and the size distribution.