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.
| Well-Preserved 6-Kilometer Diameter Crater: ESP_020807_2055 ESP_021664_2055 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 25.33 | 94.6 | 0.74 | 22.70 | 63.6 | 64.3 |
| Fresh 2-Kilometer Diameter Impact Crater Northwest of Hellas Planitia: ESP_020598_1490 ESP_020875_1490 (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 | -30.8 | 47.1 | 7.13 | -18.7 | 56.2 | 54.7 |
| Central Structure of Large Impact Crater: ESP_020695_1440 ESP_029398_1440 (Interval in Earth days: 678) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.5 | 280. | -0.9 | 26.38 | 56.6 | 55.8 |
| Possible Oudemans Crater-Related Deposits Emplaced into Valles Marineris: ESP_020880_1705 ESP_020814_1705 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.19 | 267. | -19. | 3.696 | 54.4 | 53.0 |
| Central Uplift in 20-Kilometer Diameter Crater: ESP_020472_1475 ESP_068024_1475 (Interval in Earth days: 3705) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -32.3 | 247. | 5.07 | -11.7 | 58.2 | 51.4 |
| Sinuous Ridges in the Aeolis/Zephyria Region: ESP_020528_1750 ESP_020673_1750 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.06 | 154. | 7.87 | 22.67 | 54.0 | 52.4 |
| Fan and Valley within Crater: ESP_020323_2050 ESP_020824_2050 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.54 | 348. | -1.3 | 18.52 | 59.4 | 62.1 |
| Potential Future Mars Landing Site in Melas Chasma: ESP_020286_1700 ESP_020708_1700 (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 | -9.88 | 283. | -0.7 | -17.3 | 55.5 | 55.2 |
| Phyllosilicates in Bedrock of Eastern Coprates Chasma: ESP_020259_1670 ESP_020681_1670 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.9 | 301. | -2.7 | -19.5 | 56.2 | 55.4 |
| A Classic Bowl on Mars: ESP_020245_2190 ESP_020667_2190 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.68 | 316. | 2.71 | -9.81 | 63.2 | 69.5 |
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