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.
| Shallow Channels Entering Collapse Terrain near Orson Welles Crater: ESP_066979_1780 ESP_073877_1780 (Interval in Earth days: 537) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -1.90 | 313. | -5.2 | 10.09 | 42.0 | 55.8 |
| Gully Monitoring and Topography: ESP_067155_1415 ESP_074132_1415 (Interval in Earth days: 543) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.3 | 195. | 5.52 | 26.12 | 41.5 | 49.6 |
| Flow-Like Feature within Adamas Labyrinthus: ESP_067290_2195 ESP_067422_2195 (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 | 39.14 | 101. | 7.82 | -6.03 | 62.5 | 61.6 |
| Channel in Margaritifer Terra: ESP_066965_1680 ESP_067783_1680 (Interval in Earth days: 64) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.0 | 336. | -0.0 | 13.94 | 38.6 | 39.3 |
| Large New Impact Crater: ESP_066951_2150 ESP_084385_2150 (Interval in Earth days: 1358) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 34.67 | 352. | -1.0 | 24.80 | 64.3 | 64.4 |
| Flow Surface with Cones in Tartarus Colles: ESP_067050_2070 ESP_067591_2070 (Interval in Earth days: 42) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 26.78 | 172. | -4.5 | -16.3 | 57.5 | 52.4 |
| Gullies Emanating from Lobate Flow: ESP_067296_1315 ESP_058856_1315 (Interval in Earth days: 658) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -48.0 | 309. | 9.71 | -12.4 | 47.6 | 50.0 |
| Valleys in Crater Northeast of Argyre Region: ESP_067229_1500 ESP_067361_1500 (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 | -29.7 | 334. | 7.83 | -10.6 | 39.0 | 41.4 |
| Steep Rocky Slopes in Central Valles Marineris: ESP_067257_1665 ESP_066439_1665 (Interval in Earth days: 64) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.1 | 290. | -15. | 6.069 | 39.2 | 41.7 |
| Dipping Layers in Crater in Southern Mid-Latitudes: ESP_067118_1415 ESP_067659_1415 (Interval in Earth days: 42) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.3 | 125. | 2.08 | -7.47 | 41.5 | 48.5 |
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