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.
| Fresh or Well-Preserved Chain of Impact Craters in Hesperia Planum: PSP_009572_1620 ESP_016231_1620 (Interval in Earth days: 519) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -17.6 | 109. | -3.3 | 21.86 | 66.2 | 52.1 |
| Head of Small Chasma on Edge of North Polar Layered Deposits: PSP_010079_2625 PSP_010105_2625 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 82.53 | 284. | -8.6 | 4.489 | 65.1 | 64.6 |
| Landslide Deposit in Ophir Chasma: PSP_009750_1760 PSP_009895_1760 (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 | -3.80 | 288. | -4.3 | 12.25 | 58.0 | 56.8 |
| Double Crater on Cerberus Plains: PSP_009860_1805 ESP_042892_1805 (Interval in Earth days: 2574) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.433 | 164. | -5.2 | -19.3 | 56.0 | 46.7 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_010163_2675 PSP_010230_2675 (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 | 87.26 | 123. | -8.3 | -20.4 | 69.1 | 70.5 |
| Central Peak and Pit with Bedrock Exposures: PSP_010389_1670 ESP_025751_1670 (Interval in Earth days: 1197) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.9 | 123. | 4.69 | -15.0 | 61.2 | 57.5 |
| Central Uplift of Hargraves Crater in the Nili Fossae Region: PSP_009639_2010 PSP_010272_2010 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 20.73 | 75.8 | -5.4 | -21.0 | 47.8 | 52.1 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_010139_2675 PSP_010483_2675 (Interval in Earth days: 27) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.32 | 55.3 | -8.6 | -21.3 | 68.8 | 73.9 |
| Hydrated Light-Toned Layers on Crater Floor: PSP_010274_2140 PSP_010696_2140 (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 | 33.63 | 17.0 | 5.05 | -8.32 | 49.3 | 54.8 |
| Bedrock Layers Exposed in Northern Hellas Basin: PSP_009389_1510 PSP_010022_1510 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.8 | 67.0 | 0 | -18.6 | 73.7 | 73.1 |
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