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.
| Candidate Future Landing Site at Valley North of Jezero Crater: ESP_032794_1990 ESP_033216_1990 (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 | 19.03 | 77.3 | 7.33 | -15.0 | 38.0 | 38.9 |
| Sand Patch Southwest of Medusae Fossae: ESP_032500_1715 ESP_032777_1715 (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 | -8.24 | 187. | 3.55 | -26.3 | 32.9 | 37.4 |
| Possible Hydrated Silicates in Acidalia Planitia: ESP_032850_2200 ESP_033641_2200 (Interval in Earth days: 61) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.91 | 347. | -6.6 | 21.87 | 50.4 | 41.9 |
| Sharp-Looking High-Latitude Gullies: ESP_032560_1300 ESP_032692_1300 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -49.7 | 355. | -0.0 | -29.5 | 54.0 | 58.1 |
| Gullied Crater: ESP_032883_1400 ESP_033173_1400 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -39.6 | 175. | -2.3 | 16.04 | 52.4 | 56.3 |
| Eroded Crater: ESP_032585_1870 ESP_033086_1870 (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 | 6.825 | 25.6 | -1.1 | 16.26 | 35.0 | 34.5 |
| Viscous Flow: ESP_032875_2195 ESP_033165_2195 (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 | 39.34 | 24.7 | -7.0 | 8.757 | 49.7 | 45.9 |
| USGS Dune Database Number 0284-520 Changes: ESP_032783_1275 ESP_033060_1275 (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 | -52.0 | 28.5 | -3.4 | -25.7 | 59.8 | 65.9 |
| Migrating and Static Sand Ripples on Mars: ESP_032616_1275 ESP_032748_1275 (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 | -52.2 | 267. | 3.02 | -26.0 | 56.8 | 60.7 |
| Lava against an Impact Crater in Elysium Planitia: ESP_018537_1860 ESP_019170_1860 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 5.980 | 150. | 5.55 | -19.2 | 51.1 | 53.8 |
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