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.
| Pasteur Crater Mound with Exposed Layers: ESP_013544_1995 ESP_013610_1995 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.19 | 24.0 | -4.4 | -23.3 | 57.5 | 57.9 |
| Possible Fan Delta: ESP_013531_2140 ESP_022036_2140 (Interval in Earth days: 663) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 33.87 | 17.5 | -8.5 | 21.35 | 68.7 | 68.8 |
| Terraced Double Crater in Margaritifer Sinus: ESP_014152_1505 ESP_014429_1505 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -29.3 | 350. | -5.5 | -28.3 | 35.3 | 38.5 |
| Light-Toned Outcrop in Hummock of Iani Chaos: ESP_013717_1790 ESP_013862_1790 (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 | -1.05 | 342. | 5.13 | 18.19 | 42.1 | 39.5 |
| Basal Exposure of South Polar Layered Deposits: ESP_013290_1075 ESP_013092_1075 (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 | -72.2 | 138. | -18. | 5.428 | 55.8 | 55.0 |
| Flood Lava Passing through a Constriction in Amazonis Planitia: ESP_014184_2070 ESP_020276_2070 (Interval in Earth days: 475) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 26.88 | 190. | -8.6 | 13.66 | 54.9 | 58.4 |
| Edge of Fluidized Ejecta Rampart with Great Phyllosilicate Signature: ESP_012909_1680 ESP_013331_1680 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.9 | 83.6 | 3.17 | -12.0 | 47.1 | 43.1 |
| Well-Preserved Gullied Impact Crater: ESP_013962_1430 ESP_021676_1430 (Interval in Earth days: 601) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -36.7 | 138. | 0.22 | -12.7 | 36.6 | 43.8 |
| Differential Erosion of Light-Toned Stratigraphy in Melas Chasma: ESP_013640_1710 ESP_012928_1710 (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 | -8.93 | 285. | 8.51 | -10.3 | 39.1 | 48.9 |
| 10 Kilometer Diameter Rayed Crater: ESP_012738_1785 ESP_013094_1785 (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 | -1.41 | 70.8 | 2.49 | 14.97 | 53.0 | 48.7 |
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