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.
Basal Exposure of South Polar Layered Deposits: ESP_013145_1070 ESP_013277_1070 (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 | -73.0 | 133. | 0.46 | -14.5 | 55.6 | 56.1 |
Exposure of Layered Sequence in Terby Crater: ESP_013160_1530 ESP_074031_1530 (Interval in Earth days: 4743) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -26.9 | 74.0 | -8.4 | 2.702 | 41.5 | 52.0 |
Steep Lobate Scarps in Kasei Valles: ESP_012717_1910 ESP_013139_1910 (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 | 10.88 | 282. | 2.07 | -8.93 | 59.1 | 56.6 |
Possible Olivine-Rich Terrain in Ejecta of a Gullied Crater: ESP_012761_1430 ESP_013117_1430 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -36.8 | 167. | 6.94 | 17.27 | 45.6 | 40.1 |
Landslides at the Edge of the South Polar Layered Deposits: ESP_013026_1080 ESP_013224_1080 (Interval in Earth days: 15) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -71.9 | 143. | -8.2 | -28.8 | 56.2 | 56.7 |
Gullies: ESP_012734_1265 ESP_012879_1265 (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 | -53.1 | 188. | -7.8 | 2.791 | 50.7 | 47.9 |
Comparative Gully Morphology: ESP_013934_1335 ESP_014000_1335 (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 | -46.0 | 183. | 6.35 | -11.3 | 40.0 | 41.5 |
Bedrock Exposures in Central Uplift of Large Crater North of Eos Chasma: ESP_013151_1685 ESP_013573_1685 (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 | -11.2 | 317. | -0.6 | -17.0 | 44.8 | 40.9 |
Crater between Branches of Athabasca Valles: ESP_013460_1900 ESP_013737_1900 (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 | 9.648 | 157. | 4.42 | -23.9 | 51.5 | 50.0 |
Central Structure of Verlaine Crater: ESP_013213_1705 ESP_013635_1705 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.25 | 64.1 | -1.2 | -15.7 | 44.8 | 40.8 |
Page 633 of 784 (7,833 images) |