CTX orbital imagery with a HiRISE rover-site mosaic where coverage is available. Tile gaps remain transparent.
NASA Mars Trek WMTS ↗Navigate Mars
with evidence.
Choose a landing site anywhere on Mars, inspect ARES destination candidates within 5 km, and compare a traverse with the available terrain and environment evidence.
Choose a landing site anywhere on Mars.
Start with the full planet. Tap the map or enter coordinates; ARES screens nearby destination candidates within 5 km.
MAP LAYERS4 / 8 ON⌄
Review destinations around your landing site.
The astronaut’s landing point anchors eight candidate destinations. ARES ranks the available evidence; choose any unblocked candidate to open its route review.
Select a landing point on page 2
No coordinates selected
Location reference: awaiting astronaut-selected landing point. Open source ↗
The astronaut selects the landing site. ARES scores possible destinations inside the 5 km radius using available terrain texture, model wind/dust, path distance and marked exclusions.
How the provisional rank works: candidate screen score combines available MOLA texture, modeled wind exposure, dust opacity and distance. Missing evidence is not treated as proof of safety. Wind, dust, pressure and temperature may repeat because NASA’s global model is coarse; only operator-marked obstacles are hard exclusions.
Available for context at each generated coordinate. Grid spacing varies with latitude and is far too coarse to distinguish safe conditions across a 5 km circle.
Operator-marked circles block candidate points they overlap and are hard exclusions in A*. Orbital imagery does not automatically detect obstacles.
Range uses Mars-sphere great-circle distance. Terrain is a relative MOLA image-texture proxy, not numeric elevation, slope, or a validated hazard map.
USGS geology and TES mineral layers are regional/coarse overlays. They do not establish a local mineral detection or rank 5 km sites for safety.
Decision boundary: ARES can identify marked exclusions and compare relative map-texture and distance inputs. It has no mission-approved crew thresholds, local weather forecast, or complete obstacle inventory; every candidate remains HOLD FOR HUMAN REVIEW.
Check conditions at the destination.
ARES refreshes the NASA model fields whenever the destination pointer moves.
Latest surface report
Gale measurements describe the rover station, not every point on a traverse. Downlink timing and missing fields can limit freshness.
Destination model fields
Selected destination · loading
Route inputs · editable by mission team
Waiting for destination model vector
The NASA grid returns 36 × 60 global model fields (about 300 km per cell near Gale), so it cannot resolve a kilometer-scale traverse or identify a passing dust front. The default Mars Explorer page describes its model as EMARS MY32 moderate-dust climatology and says the app is for testing. Its grid response has no forecast-valid timestamp. Dust opacity is displayed as τ; ARES does not label it an active storm or use a NASA safety threshold.
Follow the water-shaped rock record.
Use the Pahrump Hills evidence as a geological objective; keep broad orbital context separate from a local mineral claim.
Select a destination candidate
—ARES surfaces published site context for mission review. It does not identify a fresh outcrop or infer a mineral detection from the global TES layer.
Water-related sedimentary context
NASA describes sedimentary rocks at Pahrump Hills as rocks scientists believe formed in the presence of water.
NASA · Curiosity at Pahrump Hills ↗HiRISE scene context
The ESP_039280_1755 product centers on the Pahrump Hills area. Its image supports visual terrain inspection; it does not certify traversability.
HiRISE product · ESP_039280_1755 ↗Global units, coarse scale
USGS SIM 3292 maps Mars at 1:20,000,000. ARES shows the tile for regional orientation only; local contacts require finer mapping.
USGS · Geologic Map of Mars ↗TES spectral context
Sheet-silicate / high-silica-glass context is very coarse and can be confused with dust. It is not a Pahrump mineral identification.
NASA Mars Trek · TES metadata ↗Curiosity’s proposed Mount Sharp path
NASA’s rover route is a science-planning precedent built from orbital observations. It is not plotted as ARES’s route and makes no human-safety claim.
NASA · Curiosity route proposal ↗Review the route to your destination.
You choose the landing site; ARES ranks a nearby destination within 5 km. Compare the shortest and environment-weighted paths, checkpoints and data behind the provisional ranking.
Evaluating available conditions…
The route is a model ranking only. Waiting for map and condition inputs.
Shortest path
Environment-weighted path
Pressure, temperature, and mineral data are surfaced in the decision record. They are not converted into unsupported local safety thresholds or mineral detections.
Waiting for destination selection
Choose a start and destination on page 2 to compare the two route candidates.
NASA global atmosphere grid samples are coarse regional context, not a local weather forecast. Mineral and obstacle coverage is incomplete.
When conditions change, pause and replan.
ARES demonstrates the response logic while keeping mission control and crew limits authoritative.
Wind, dust, or an obstacle changes.
Enter a current model or station value, or mark a newly observed exclusion area on the map.
ARES recalculates both paths.
A* treats marked obstacle circles as hard blocks; wind and dust inputs change the relative route cost.
Mission control reviews the hold gate.
Confirm live conditions, life-support margins, suit/EVA rules, communications and crew status outside this prototype.