Planned stereo pairs have suitable stereo convergence angles and illumination by design.
In addition to planned stereo pairs, the Pairendipity software can identify overlapping
HiRISE images that are serendipitously suitable for stereo processing and find stereo
pairs within the CTX dataset.
Planned HiRISE stereo pairs are listed in the “Stereo Pair List (CSV)” link below.
Since this list is based on produced stereo anaglyphs it also contains a few serendipitous
pairs that underwent special processing. Most serendipitous HiRISE stereo pairs are listed
in the “Pairendipity Stereo” link, while CTX stereo pairs are listed
in “Pairendipity CTX Stereo”.
Images taken close together in time minimize illumination and frost differences and are
especially useful (see the Delta-Days column in the Pairendipity files or difference
the orbit numbers in the image IDs in the Stereo Pair List file). Stereo pairs
with both images planned within the same 14-day (168-orbit) operations cycle are known as SPORCs.
| Gullies Cut into Light-Toned Rock: PSP_006888_1410 ESP_016184_1410 (Interval in Earth days: 724) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.4 | 319. | 2.83 | -23.2 | 59.4 | 68.2 |
| Seasonal Monitoring: PSP_005750_0965 PSP_005921_0965 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -83.6 | 99.6 | -2.1 | 13.97 | 75.7 | 77.5 |
| Layered Rock Outcrops in West Candor Chasma: PSP_005742_1750 PSP_006665_1750 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.93 | 285. | 1.77 | -8.25 | 33.5 | 39.1 |
| Sinuous Ridge in Argyre Basin: PSP_006730_1235 PSP_007007_1235 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -56.1 | 316. | 7.79 | -14.4 | 69.5 | 75.4 |
| Oblique Impact Exposing Bedrock within A Libya Montes Massif: PSP_005934_1845 ESP_013766_1845 (Interval in Earth days: 611) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.265 | 81.9 | 4.88 | 28.69 | 35.1 | 42.8 |
| Pair of Odd Craters of Hrad Vallis Deposit: PSP_006881_2145 PSP_010375_2145 (Interval in Earth days: 272) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 34.25 | 141. | 6.74 | -8.95 | 42.8 | 51.5 |
| Light-Toned Layers in Noctis Labyrithus: PSP_006890_1695 ESP_015975_1695 (Interval in Earth days: 708) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -10.4 | 261. | 2.52 | -22.8 | 42.9 | 48.0 |
| Gorgonum Chaos: PSP_006906_1425 ESP_016004_1425 (Interval in Earth days: 709) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.2 | 188. | 1.20 | 29.59 | 58.9 | 61.5 |
| Intersecting Troughs in Lycus Sulci: PSP_006285_2000 ESP_032789_2000 (Interval in Earth days: 2065) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.66 | 216. | 0 | -24.1 | 39.9 | 40.8 |
| Large Crater on South Polar Layered Deposits: PSP_005695_1015 PSP_005603_1015 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -78.2 | 146. | -0.6 | -21.2 | 69.9 | 69.8 |
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