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.
| Wall of Orson Welles Crater: ESP_035594_1790 ESP_071042_1790 (Interval in Earth days: 2761) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -0.76 | 314. | 0 | 19.68 | 54.9 | 57.3 |
| Possible Terraced Crater in Arcadia Planitia: ESP_035532_2195 ESP_035809_2195 (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 | 38.98 | 202. | -2.9 | -20.4 | 42.5 | 45.2 |
| Monitoring Active Dunes in Arabia Terra: ESP_035315_1865 ESP_036027_1865 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 6.197 | 11.6 | -6.9 | 20.99 | 51.0 | 50.4 |
| 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 |
| Exposure of North Polar Layered Deposits: ESP_035567_2650 ESP_035909_2650 (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 | 84.92 | 294. | 0.21 | 15.65 | 60.1 | 60.9 |
| Crater on Wall in Mamers Valles: ESP_035341_2195 ESP_035631_2195 (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 | 39.35 | 16.4 | 3.18 | 25.38 | 41.5 | 40.2 |
| 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 |
| Channels in Nilokeras Mensae: ESP_035449_2100 ESP_071741_2100 (Interval in Earth days: 2828) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 29.56 | 309. | 2.31 | -8.62 | 42.5 | 49.2 |
| Landform Transition from Chaos Terrain to Outflow Channel: ESP_035475_1830 ESP_036042_1830 (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 | 2.839 | 323. | -6.8 | 6.109 | 53.2 | 53.2 |
| Outflow Deposit from Hrad Vallis: ESP_035376_2145 ESP_034031_2145 (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 | 34.04 | 141. | 1.79 | 14.40 | 41.9 | 39.4 |
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