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.
| Scarp Fronted Deposit in South Gunjur Crater: ESP_066774_1795 ESP_067526_1795 (Interval in Earth days: 59) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -0.32 | 146. | 8.48 | 17.64 | 43.5 | 38.5 |
| Gullied Slope: ESP_066775_1425 ESP_066841_1425 (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 | -37.2 | 124. | 8.23 | -2.84 | 39.0 | 39.9 |
| Landforms in Terra Sabaea: ESP_066541_1855 ESP_066475_1855 (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 | 5.645 | 25.8 | -8.5 | 5.876 | 50.2 | 50.0 |
| Small Shield Volcano North of Noctis Labyrinthus: ESP_066572_1825 ESP_066783_1825 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.527 | 259. | -1.9 | 21.85 | 47.7 | 43.9 |
| Elongating Linear Dunes in Argyre Planitia: ESP_066808_1330 ESP_066610_1330 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -46.8 | 305. | 2.41 | 28.89 | 43.0 | 40.3 |
| Craters with Steep Slopes: ESP_066516_1445 ESP_084570_1445 (Interval in Earth days: 1407) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.1 | 352. | 1.33 | 7.927 | 39.4 | 36.6 |
| Oyama Crater: ESP_066780_2040 ESP_066991_2040 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.79 | 340. | -1.6 | 21.25 | 58.6 | 54.7 |
| Tilted Strata in Central Structure of Martin Crater: ESP_066848_1585 ESP_067798_1585 (Interval in Earth days: 74) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.4 | 290. | -0.1 | -9.63 | 37.8 | 43.4 |
| Features in Iani Chaos: ESP_066503_1795 ESP_066569_1795 (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 | -0.27 | 342. | 7.35 | -6.95 | 46.4 | 46.7 |
| Channel-Like Features in Cerberus Region: ESP_066589_1935 ESP_075175_1935 (Interval in Earth days: 668) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 13.50 | 153. | 9.00 | 7.223 | 53.3 | 54.5 |
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