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.
| Crater Exposing Layers in Icy Deposits: ESP_089851_2175 ESP_090128_2175 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 36.92 | 161. | 8.87 | -6.46 | 51.8 | 56.4 |
| Volcanic Cones in Ceraunius Fossae: ESP_089650_2050 ESP_089927_2050 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.57 | 250. | 6.19 | -14.8 | 49.8 | 53.6 |
| Closed Fretted Terrain Valley: ESP_089724_2185 ESP_089790_2185 (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 | 38.34 | 28.0 | 6.60 | -9.01 | 50.9 | 52.9 |
| Barchan to Sand Sheet Transition in Central Herschel Crater: ESP_089892_1655 ESP_090037_1655 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.1 | 129. | -3.4 | 17.28 | 62.1 | 60.1 |
| Double Crater: ESP_089603_2125 ESP_089880_2125 (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 | 32.26 | 93.1 | -1.8 | -20.5 | 49.9 | 54.1 |
| Glacier Layering Revealed by Impact Crater on Viscous Flow Features Surface: ESP_089764_2200 ESP_089487_2200 (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 | 39.61 | 17.6 | -8.7 | 10.06 | 52.8 | 48.4 |
| Inverted Valley and Rings near Erebus Montes: ESP_089850_2210 ESP_089217_2210 (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 | 40.73 | 187. | 7.54 | 17.77 | 52.6 | 45.6 |
| Exposed Layers in Olympia Mensae Icy Outliers: ESP_089774_2545 ESP_089787_2545 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 74.13 | 95.1 | -4.3 | 10.35 | 64.8 | 63.9 |
| Northern Gullies on Mesa: ESP_089662_2300 ESP_090216_2300 (Interval in Earth days: 44) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 49.67 | 278. | 7.68 | -17.0 | 52.5 | 62.0 |
| Scarp Contact: ESP_089889_1920 ESP_090166_1920 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 11.85 | 207. | 1.64 | -17.1 | 53.2 | 56.1 |
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