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.
| Central Peak Ring of Crater with Olivine and Diverse Bedrock Exposures: PSP_005816_1750 ESP_011512_1750 (Interval in Earth days: 444) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.95 | 64.9 | 0 | -25.3 | 33.6 | 59.6 |
| Survey South Polar Layered Deposits: PSP_004593_0830 PSP_004984_0970 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.6 | 140. | 0 | -19.2 | 72.1 | 65.8 |
| Crater of Floor of Mawrth Vallis Channel: PSP_006755_2030 ESP_011383_2030 (Interval in Earth days: 361) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.95 | 341. | 20.9 | -3.88 | 37.8 | 60.1 |
| Seasonal Monitoring: PSP_005553_0980 PSP_005790_0980 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.1 | 75.6 | -8.4 | 8.644 | 71.5 | 74.2 |
| Channels or Flow Features with Inverted Topography on Arsia Mons: PSP_005915_1720 ESP_011690_1720 (Interval in Earth days: 450) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.81 | 242. | -5.1 | 8.736 | 33.9 | 56.6 |
| Oswego Region Unfrosted: PSP_005619_0945 PSP_005803_0945 (Interval in Earth days: 14) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.4 | 83.5 | 1.81 | 17.68 | 74.9 | 76.8 |
| Crater Cut by Coprates Chasma: PSP_005148_1665 ESP_014114_1665 (Interval in Earth days: 699) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.7 | 303. | -4.6 | 22.21 | 34.6 | 32.5 |
| Layered Sediments in Tithonium Chasma: PSP_005281_1750 PSP_005703_1750 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.92 | 270. | 10.9 | -5.09 | 35.2 | 34.1 |
| Thermally-Distinct Rays Emanating from Gratteri Crater: PSP_006510_1635 ESP_020922_1635 (Interval in Earth days: 1123) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -16.3 | 197. | 0 | 27.48 | 40.6 | 49.7 |
| Lava Falls in Northern Kasei Valles: PSP_005610_2025 ESP_040659_2025 (Interval in Earth days: 2731) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.00 | 286. | -5.7 | 8.888 | 47.7 | 50.0 |
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