Ophir Chasma is a chasma — a deep, steep-sided canyon — on Mars, 315 km across, centred at 4.0° S, 72.4° W in the Coprates quadrangle. It is the 308th largest named feature on Mars and the 14th largest of its class there.
Classical albedo feature name. The International Astronomical Union approved the name in 1973, under the theme it applies to every chasma on Mars. Of the 25 features of this class catalogued on Mars, the naming categories run Greek (13), Latin (12).
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 4.0° S, 72.4° W.
What this spot has going for it is sunlight — 100% of the sunlight the sunniest latitude on Mars gets. What works against it is water — outside the ice-bearing latitudes.
Computed from Ophir Chasma'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.
All 25 chasmata on Mars — mapped together, with the naming theme and the size distribution.