1 00:00:00,800 --> 00:00:02,235 Mars 2020 Landing Site: Jezero Crater Flyover 2 00:00:06,605 --> 00:00:10,309 This flyover was produced from NASA images taken from orbit. 3 00:00:10,342 --> 00:00:14,080 The blue circle indicates the area the rover will likely land. 4 00:00:14,113 --> 00:00:17,450 The arcing hills in the center, about 1600 feet high, 5 00:00:17,483 --> 00:00:19,786 and are the rim of Jezero Crater. 6 00:00:19,819 --> 00:00:21,621 The goal of Mars 2020 is to learn 7 00:00:21,654 --> 00:00:23,923 whether life ever existed on Mars. 8 00:00:23,956 --> 00:00:26,092 It's too cold and dry for life to exist 9 00:00:26,125 --> 00:00:27,960 on the Martian surface today. 10 00:00:27,993 --> 00:00:30,963 But after Jezero Crater formed billions of years ago, 11 00:00:30,996 --> 00:00:33,266 water filled it to form a deep lake 12 00:00:33,299 --> 00:00:36,135 about the same size as Lake Tahoe. 13 00:00:36,168 --> 00:00:40,773 Eventually, as Mars' climate changed, Lake Jezero dried up. 14 00:00:40,806 --> 00:00:43,810 And surface water disappeared from the planet. 15 00:00:43,843 --> 00:00:47,080 An ancient lake is a fantastic place to pursue our goal 16 00:00:47,113 --> 00:00:49,482 of looking for possible Martian life. 17 00:00:49,515 --> 00:00:52,251 On Earth, lakes are filled with living creatures. 18 00:00:52,284 --> 00:00:55,188 Evidence of that life is often preserved in the mud and sand 19 00:00:55,221 --> 00:00:57,323 deposited on the bottom of the lake. 20 00:00:57,356 --> 00:00:59,492 So we use the rover's instruments to explore 21 00:00:59,525 --> 00:01:01,761 the rocks of the ancient lake bed. 22 00:01:02,762 --> 00:01:05,164 Here we can see evidence of the former lake. 23 00:01:05,197 --> 00:01:07,233 A canyon cutting through the crater rim 24 00:01:07,266 --> 00:01:09,102 was carved by a river. 25 00:01:09,135 --> 00:01:11,104 As the water entered the lake it slowed 26 00:01:11,137 --> 00:01:13,039 and dropped the sand and mud it was carrying 27 00:01:13,072 --> 00:01:15,075 to form the fan-shaped delta. 28 00:01:16,042 --> 00:01:18,177 The white line is a path the rover might follow 29 00:01:18,210 --> 00:01:21,147 in its first two years, called the prime mission. 30 00:01:21,180 --> 00:01:23,850 During this period we use the rover science instruments 31 00:01:23,883 --> 00:01:26,152 to analyze the lake sediments. 32 00:01:26,385 --> 00:01:28,020 After we explore the delta, 33 00:01:28,053 --> 00:01:31,091 we hope to investigate the shoreline of the former lake. 34 00:01:31,825 --> 00:01:33,359 To get there we have to traverse around 35 00:01:33,392 --> 00:01:35,528 a sea of modern sand dunes. 36 00:01:35,661 --> 00:01:38,197 From this perspective you can see former shorelines 37 00:01:38,230 --> 00:01:39,966 curving around a headland. 38 00:01:39,999 --> 00:01:43,903 We can picture waves in Lake Jezero beating on a sandy beach. 39 00:01:44,670 --> 00:01:47,140 And finally we will press on to the crater rim. 40 00:01:48,408 --> 00:01:50,543 Jezero Crater formed when a large object collided with Mars, 41 00:01:50,576 --> 00:01:53,012 excavating rocks from deep in the Martian crust, 42 00:01:53,045 --> 00:01:55,582 exposing them in the rim for us to study. 43 00:01:56,249 --> 00:01:58,885 These rocks would have been hot shortly after the impact 44 00:01:58,918 --> 00:02:00,820 and may have hosted hot springs. 45 00:02:00,853 --> 00:02:02,855 Deposits from these springs would be another target 46 00:02:02,888 --> 00:02:05,892 in our search for possible ancient life on Mars. 47 00:02:10,462 --> 00:02:12,098 NASA Jet Propulsion Laboratory