ライブ
Mars · Labyrinthus · 593rd largest named feature

Hyperboreus Labyrinthus

Classical albedo feature name.

What Hyperboreus Labyrinthus is

Hyperboreus Labyrinthus is a labyrinthus — a complex of intersecting valleys or ridges — on Mars, 112 km across, centred at 80.3° N, 59.8° W in the Mare Boreum quadrangle. It is the 593rd largest named feature on Mars and the 4th largest of its class there.

Where the name comes from

Classical albedo feature name. The International Astronomical Union approved the name in 1988, under the theme it applies to every labyrinthus on Mars. Of the 6 features of this class catalogued on Mars, the naming categories run Latin (3), Greek (2), Romania (Rumania) (1).

Feature class
a complex of intersecting valleys or ridges
Diameter
112 km
about the width of Yellowstone
Coordinates
80.3° N, 59.8° W
Planetocentric, on Mars
Name approved
1988
By the IAU Working Group for Planetary System Nomenclature
Quadrangle
Mare Boreum
Map sheet on Mars
Naming category
Romania (Rumania)
Europe

What it would take to settle Hyperboreus Labyrinthus

Mars scores 26.6 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 80.3° N, 59.8° W.

Settlement difficulty here
27.7/ 100
Typical for this world
Mars overall
26.6
1.1 harder than the median site
Ranked
1735th
of 2,049 named places on Mars

What this spot has going for it is water inside the polar zone where Mars keeps its ice. What works against it is ground broken ground — hard to reach, and worth reaching for the shelter and the exposed strata.

Computed from Hyperboreus Labyrinthus's catalogued latitude, longitude and feature class — 74% of the model's weight had a basis here, and 2 axes were dropped as not applicable to Mars (radiation geometry, earth link). Gravity, pressure, delta-v and distance from the Sun are the same everywhere on Mars 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 labyrinthus features on Mars