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.
| Valleys Cut in Bedrock: PSP_009082_1605 ESP_053665_1605 (Interval in Earth days: 3474) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.1 | 166. | 5.29 | -7.86 | 66.6 | 64.3 |
| Tube-Fed Lava Flow Field: PSP_008433_1755 PSP_009501_1755 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.58 | 247. | 7.65 | -15.8 | 54.7 | 59.2 |
| Tongue-Shaped Feature on Slope Seen in MOC Images R04-02106 and R12-01135: PSP_008519_2210 PSP_009020_2210 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.73 | 52.4 | 7.81 | -1.65 | 41.2 | 42.8 |
| Arcadia Planitia Domes: PSP_008554_2170 PSP_008765_2170 (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 | 36.67 | 177. | 4.87 | -13.3 | 41.4 | 43.3 |
| Mounds on Lineated Valley Fill: PSP_008308_2160 PSP_008888_2160 (Interval in Earth days: 46) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.70 | 57.0 | -6.7 | 3.944 | 42.1 | 42.1 |
| Basal Units in North Polar Region: PSP_009134_2645 PSP_009687_2645 (Interval in Earth days: 43) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.66 | 157. | -7.5 | 10.32 | 60.3 | 62.1 |
| Deposits Layered at Several Scales: PSP_009038_1745 PSP_010027_1745 (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 | -5.54 | 286. | 2.43 | -12.1 | 58.0 | 59.4 |
| Inverted Riverbed in Gale Crater: PSP_009149_1750 PSP_009294_1750 (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 | -4.79 | 137. | -12. | 2.236 | 58.8 | 57.9 |
| Chloride Salt Deposits within a Channel in Terra Sirenum : PSP_009318_1465 ESP_017243_1465 (Interval in Earth days: 618) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -33.4 | 205. | 6.27 | -8.10 | 76.6 | 74.7 |
| Transverse Dunes in the Northern Lowlands: PSP_008681_2550 PSP_009195_2550 (Interval in Earth days: 40) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 74.98 | 300. | -2.3 | 10.88 | 54.3 | 53.4 |
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