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.
| Ring of Cratered Cones: ESP_035098_2065 ESP_034808_2065 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 26.23 | 170. | 22.2 | 0 | 40.4 | 41.6 |
| Light-Toned and Swirly Deposits along Floor of Coprates Catena Trough: ESP_035410_1655 ESP_034988_1655 (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 | -14.5 | 299. | 6.08 | 21.52 | 62.7 | 60.1 |
| Impact Monitoring Site in Phlegra Montes: ESP_035362_2190 ESP_060984_2190 (Interval in Earth days: 1997) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.72 | 163. | -3.3 | -21.8 | 42.2 | 41.7 |
| Lava Channels in Tartarus Montes: ESP_035586_2050 ESP_036364_2050 (Interval in Earth days: 61) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.73 | 170. | -1.9 | 13.12 | 44.3 | 46.0 |
| InSight Mission Candidate Landing Site: ESP_035495_1835 ESP_035429_1835 (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 | 3.303 | 138. | -13. | 9.156 | 53.4 | 51.7 |
| Xanthe Terra Region: ESP_035528_1920 ESP_036873_1920 (Interval in Earth days: 105) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 11.66 | 315. | 0.16 | 11.08 | 48.5 | 51.2 |
| North Polar Layered Deposit Exposure: ESP_035572_2665 ESP_036008_2665 (Interval in Earth days: 34) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 86.54 | 138. | 0.38 | -10.4 | 61.4 | 63.3 |
| Double-Terraced Crater next to Single-Terraced Crater in Arcadia Planitia: ESP_035545_2290 ESP_036455_2290 (Interval in Earth days: 71) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 48.74 | 206. | -4.8 | -18.2 | 43.8 | 50.5 |
| Sediment Routing System in Aeolis Dorsa: ESP_035455_1780 ESP_036800_1780 (Interval in Earth days: 104) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -1.78 | 149. | 4.58 | 17.96 | 54.9 | 54.7 |
| Erosional Morphologies in Outflow Channel Bend of Shalbatana Vallis: ESP_035396_1890 ESP_037097_1890 (Interval in Earth days: 133) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 8.680 | 319. | 4.05 | 19.88 | 49.2 | 51.9 |
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