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.
Survey Layering and Faulting in Layered Deposits in Candor Chasma: PSP_009328_1755 PSP_010172_1755 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.38 | 288. | 5.36 | -21.3 | 57.5 | 59.5 |
Tooting Crater Southern Ejecta Layer: PSP_009766_2030 PSP_009832_2030 (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 | 22.53 | 207. | 2.91 | -16.9 | 47.2 | 49.2 |
North Polar Terrain: PSP_009914_2750 PSP_010682_2650 (Interval in Earth days: 59) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.90 | 334. | 0 | 18.02 | 69.7 | 73.7 |
Multiple Unconformities in the Upper North Polar Layered Deposits: PSP_010181_2600 PSP_010234_2600 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 79.74 | 23.4 | -6.9 | -18.7 | 64.6 | 66.2 |
Stratigraphy in the Nili Fossae Noachian Crust: PSP_009494_2010 PSP_010127_2010 (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 | 20.52 | 73.7 | 3.21 | -14.8 | 46.7 | 50.7 |
Western Half of Heimdal Crater: PSP_009580_2485 PSP_009778_2485 (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 | 68.34 | 235. | 4.49 | -17.3 | 52.3 | 55.5 |
Fluvial and Alluvial Features on North Wall of Eos Chasma: PSP_009894_1665 PSP_010606_1665 (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 | -13.3 | 317. | 3.44 | 21.18 | 62.6 | 59.5 |
Exposure of Polar Layered Deposits in Area Not Well Observed: PSP_009347_2715 PSP_009388_2685 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.72 | 12.7 | -15. | -15.5 | 64.8 | 64.4 |
Exposure of Polar Layered Deposits on Ridges and Troughs: PSP_009969_2630 PSP_010008_2630 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 82.92 | 40.8 | -1.7 | 15.24 | 63.7 | 63.3 |
Debris Flow in Juventae Chasma: PSP_010198_1755 ESP_016290_1755 (Interval in Earth days: 474) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.25 | 297. | 0.26 | 22.12 | 57.8 | 45.2 |
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