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.
| Finely Stratified Units in Northeast of Gale Crater with Possible Clays: ESP_020555_1755 ESP_047139_1755 (Interval in Earth days: 2071) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.48 | 138. | 3.93 | 24.21 | 54.3 | 49.2 |
| 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 |
| Dunes on Crater Floor: ESP_020709_1350 ESP_020854_1350 (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 | -44.4 | 259. | -4.8 | 8.47 | 59.5 | 56.3 |
| Streamlined Form Surrounded by Pitted Materials in Hale Crater: ESP_020667_1440 ESP_030069_1440 (Interval in Earth days: 733) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.5 | 324. | -1.4 | -14.8 | 57.0 | 49.7 |
| Ejecta of Very Well-Preserved Crater: ESP_020723_2235 ESP_064845_2235 (Interval in Earth days: 3438) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 43.26 | 225. | -4.6 | 28.28 | 72.1 | 71.8 |
| Slope Streaks on Wall of Nicholson Crater: ESP_020421_1810 ESP_081543_1810 (Interval in Earth days: 4763) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 1.037 | 195. | 7.05 | -1.74 | 54.6 | 57.9 |
| Bedrock Exposure in Landslide Scarp: ESP_020879_1670 ESP_021657_1670 (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 | -12.9 | 293. | 5.19 | -7.68 | 52.2 | 46.1 |
| Small Crater with Gullies and a Bright Fan: ESP_020897_1455 ESP_021609_1455 (Interval in Earth days: 56) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.2 | 165. | -3.8 | 6.575 | 53.8 | 43.0 |
| 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 |
| Channels and Lava Flows: ESP_020472_2010 ESP_028384_2010 (Interval in Earth days: 617) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 20.54 | 241. | -6.5 | -28.5 | 59.8 | 53.7 |
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