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.
Alcove with Bright Rocky Slope Streaks: PSP_009762_1905 PSP_009907_1905 (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 | 10.40 | 318. | -0.3 | 15.26 | 51.2 | 50.3 |
Interaction of Cratered Cone and Crater Ejecta: PSP_009906_2225 PSP_010196_2225 (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 | 42.33 | 343. | -7.7 | 14.62 | 48.0 | 48.7 |
High-Latitude Exposure of North Polar Layered Deposits: PSP_010100_2675 PSP_010457_2675 (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 | 87.29 | 32.0 | -5.8 | -15.5 | 68.3 | 73.1 |
Possible Flute Casts in Ares Vallis: PSP_009722_1960 PSP_009867_1960 (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 | 15.92 | 329. | 2.51 | 17.22 | 48.9 | 48.1 |
Unconformities in North Polar Layered Deposits: PSP_010124_2650 PSP_010242_2650 (Interval in Earth days: 9) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.81 | 128. | -7.7 | 7.364 | 67.0 | 67.7 |
Small Shield Covering the Noctis Fossae: PSP_010305_1780 PSP_010661_1780 (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 | -1.91 | 256. | -7.0 | -0.74 | 57.3 | 56.9 |
Possible Intravalley Paleolake in Shalbatana Vallis: PSP_009683_1830 PSP_010316_1830 (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 | 2.989 | 316. | -5.0 | -21.7 | 54.6 | 56.7 |
Volcanic Fissure Vent in Elysium Planitia: PSP_010269_1900 PSP_010414_1900 (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 | 9.630 | 157. | -2.2 | 14.68 | 52.9 | 52.0 |
Reading the Rock Record at Nili Fossae: PSP_010206_1975 PSP_010628_1975 (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 | 17.24 | 76.3 | -2.9 | -17.3 | 50.8 | 54.4 |
Stratigraphy of the North Polar Deposits: PSP_010198_2645 PSP_010014_2645 (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 | 84.38 | 253. | 7.14 | -7.89 | 66.8 | 65.5 |
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