In addition to planned stereo pairs, the Pairendipity software can identify all overlapping images suitable for stereo processing. Global lists of such image pairs for the HiRISE and CTX datasets are provided here ordered by latitude. Images taken close together in time minimize illumination and frost differences and are especially useful (see the Delta-Days column). Stereo images planned within the same 14-day operations cycle are known as SPORCs.
Central Structures of Crater North of Hellas Basin: ESP_012461_1515 ESP_012883_1515 (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 | -28.2 | 76.8 | 4.41 | -11.7 | 49.8 | 45.3 |
East Wall of Ritchey Crater: ESP_011780_1515 ESP_011846_1515 (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 | -28.4 | 309. | -4.3 | -23.6 | 58.8 | 59.7 |
Fresh Crater with Lots of Gullies: ESP_011672_1395 ESP_011817_1395 (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 | -40.3 | 20.1 | -7.0 | 7.602 | 63.3 | 60.3 |
Survey Layering and Faulting in Melas Chasma Layered Deposits: ESP_012361_1685 ESP_012572_1685 (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 | -11.2 | 285. | -1.6 | -11.8 | 53.2 | 52.0 |
East Portion of Flow in Harmakhis Vallis: ESP_012434_1420 ESP_012579_1420 (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 | -37.7 | 95.5 | 1.58 | 12.57 | 51.0 | 48.0 |
Well-Preserved 15-Kilometer Crater with Gullies and Pitted Ponded Material: ESP_011773_1460 ESP_011839_1460 (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 | -33.5 | 140. | 5.89 | -13.7 | 59.1 | 59.8 |
Gullies in Southern Hemisphere Crater: ESP_011661_1410 ESP_011938_1410 (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 | -38.5 | 319. | -5.4 | -27.1 | 62.8 | 60.8 |
Very Well-Preserved 9-Kilometer Crater: ESP_011818_1505 ESP_012029_1505 (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 | -29.3 | 351. | 6.39 | -0.94 | 57.7 | 55.8 |
Streamlined Form and Channel Floor in Athabasca Valles: ESP_011825_1895 ESP_012814_1895 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 9.439 | 156. | -3.5 | -16.8 | 59.8 | 59.0 |
Double Terraces around Streamlined Hills in South End of Eastern Dao Vallis: ESP_011722_1460 ESP_011577_1460 (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 | -33.8 | 94.0 | -5.9 | -20.3 | 60.8 | 63.6 |
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