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. 
			
			
| Crater with Two Concentric Central Stuctures: ESP_018282_1640 ESP_019271_1640 (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 | -15.8 | 275. | 5.65 | -11.2 | 63.6 | 61.9 | 
| Cones at Edge of North Polar Layered Deposits: ESP_018241_2595 ESP_027063_2595 (Interval in Earth days: 688) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 79.12 | 293. | -0.4 | -20.8 | 57.4 | 58.6 | 
| Exposure of North Polar Layered Deposits: ESP_018237_2720 ESP_019053_2720 (Interval in Earth days: 64) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.90 | 293. | -9.5 | -21.3 | 65.1 | 73.4 | 
| Possible MSL Rover Landing Site in Gale Crater Covering North Central Mound: ESP_018287_1755 ESP_018788_1755 (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 | -4.58 | 137. | -0.4 | 23.35 | 57.0 | 54.9 | 
| Well-Preserved 5-Kilometer Diameter Impact Crater: ESP_018478_2150 ESP_018979_2150 (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 | 34.78 | 318. | -3.5 | 13.05 | 44.5 | 46.3 | 
| High-Latitude Exposure of North Polar Layered Deposits: ESP_018318_2675 ESP_019031_2675 (Interval in Earth days: 56) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.49 | 329. | -12. | -22.1 | 63.8 | 70.6 | 
| Putative Faulting in North Polar Layers: ESP_018313_2650 ESP_018841_2650 (Interval in Earth days: 41) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.74 | 116. | -4.6 | -18.2 | 61.5 | 66.5 | 
| Rim and Ejecta of Very Fresh 7-Kilometer Diameter Impact Crater: ESP_018268_2335 ESP_033854_2335 (Interval in Earth days: 1215) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 53.34 | 289. | -4.9 | 20.21 | 46.1 | 47.4 | 
| Central Uplift of Impact Crater: ESP_018277_1620 ESP_026202_1620 (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 | -17.5 | 52.1 | 3.42 | -23.2 | 65.0 | 64.1 | 
| Dark Outcrop: ESP_018292_1780 ESP_019492_1780 (Interval in Earth days: 94) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -1.92 | 0.09 | 11.0 | -12.0 | 54.7 | 55.9 | 
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