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.
| Source of Flow Visible in CTX Image P20_008700_1787: ESP_025697_1805 ESP_037169_1805 (Interval in Earth days: 894) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.572 | 155. | -6.8 | 8.034 | 48.6 | 54.9 |
| Abalos Mensa and Abalos Scopuli Region: ESP_025665_2610 ESP_025718_2610 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 81.01 | 280. | 7.35 | -3.58 | 60.5 | 60.6 |
| Wrinkle Ridge Superimposed on Well-Preserved Crater: ESP_025468_1640 ESP_024835_1640 (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 | -15.7 | 288. | -5.8 | 12.96 | 56.2 | 47.5 |
| Reticulate Bedform Change Detection Northwest Ascraeus Mons: ESP_025667_1960 ESP_026168_1960 (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 | 15.83 | 252. | -8.4 | 18.74 | 42.3 | 42.3 |
| Eastern Meridiani Planum Layers and Landforms: ESP_025742_1815 ESP_030265_1815 (Interval in Earth days: 352) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 1.457 | 5.70 | 6.78 | 15.41 | 47.6 | 51.8 |
| Small Mounds in Chryse Planitia: ESP_025427_1995 ESP_025282_1995 (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 | 19.37 | 322. | 6.11 | -10.3 | 39.2 | 40.0 |
| Coimbra Crater Interior Layering: ESP_025571_1840 ESP_060410_1840 (Interval in Earth days: 2714) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 3.988 | 354. | -7.4 | 8.63 | 46.1 | 40.8 |
| Terby Crater: ESP_025489_1525 ESP_033625_1525 (Interval in Earth days: 634) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.4 | 75.3 | 14.5 | 0.693 | 63.2 | 56.0 |
| Finely Stratified Units in Northeast of Gale Crater: ESP_025724_1755 ESP_025579_1755 (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 | -4.54 | 137. | 5.03 | -14.8 | 50.9 | 51.1 |
| Layered Deposits in Central Pit of Large Crater: ESP_025771_1620 ESP_043586_1620 (Interval in Earth days: 1388) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -17.6 | 296. | 6.03 | 22.31 | 59.5 | 59.5 |
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