NASA Practices Mars Exploration at KilaueaPosted on Feb 21, 2017 in Information and News Releases, Main
Unknown to thousands of visitors in Hawaiʻi Volcanoes National Park, a simulated Mars landing mission unfolded on Kīlauea Volcano for two weeks in September 2016. Sadly, Matt Damon, who starred in the movie “The Martian,” was not aboard.
The 2016 work was part of NASA’s Biologic Analog Science Associated with Lava Terrains (BASALT) program.
BASALT consists of an international group of scientists, engineers, mission operators, and astronauts dedicated to furthering the human-robotic exploration of our neighboring planet, Mars. One of the main objectives of the BASALT research program is to examine how humans can effectively explore the surface of Mars for life and to understand the geologic history of the Red Planet.
Kīlauea Volcano offers landscapes that are not perfect analogs for Mars, but that come quite close.
Under special permit from Hawaiʻi Volcanoes National Park, the BASALT team of 65 scientists, engineers, computer scientists, human-machine engineering experts, and astronauts targeted the Mauna Ulu region on Kīlauea’s East Rift Zone as the Mars landing and exploration area.
The BASALT team also set up a Science Mission Control at Kīlauea Military Camp, a facility located in the National Park. Two-way voice, video and data streaming was established between this command center and the field team, which consisted of two crew members who conducted field sampling under simulated Mars mission conditions around Mauna Ulu. These communications were delayed by up to 15 minutes to mimic transmission latencies due to the great distance between Earth and Mars.
In addition to simulating Mars mission conditions, the project also evaluated the use of various mobile science platforms, hand-held devices to determine temperature and composition of rocks, and cutting-edge video and data display technologies.
The USGS Hawaiian Volcano Observatory (HVO) supported the BASALT project by hosting communication relay antennae in our observation tower. Several HVO staff members observed the operation over the course of the project and marveled at the complicated chain of decision-making that guided the astronauts’ exploration, sampling, and documentation efforts.
Hawaiian volcanoes have featured prominently in the training of American astronauts for decades. In the 1960s and 1970s, NASA used various locations on Kīlauea and the high slopes of Mauna Kea to teach Apollo astronauts volcanology and prepare them for what they might encounter on the surface of the Moon.
More recently, NASA, along with the University of Hawaiʻi and state-sponsored PISCES (Pacific International Space Center for Exploration Systems), has conducted experiments to advance the feasibility of long-term human habitation on Mars.
From 2008 to 2012, international campaigns carried out on Mauna Kea tested methods of extracting oxygen and water from volcanic cinder. Since 2012, the Hawaiʻi Space Exploration Analog and Simulation, or HI-SEAS, program has conducted long-duration isolation missions in which crews spend up to a year inside a geodesic dome located at an elevation of 2,500 m (8,200 ft) on the slope of Mauna Loa.
More than a century ago, HVO founder Thomas A. Jaggar enthusiastically promoted the active volcanoes of Hawaiʻi as a world-class scientific laboratory. While he may not have imagined Kīlauea as a training ground for future space explorers, he almost certainly would have approved. In fact, we expect he’d argue that the first astronaut to roam the surface of the Red Planet should be a volcanologist trained on the Island of Hawaiʻi!
Prior to the BASALT program at Kīlauea Volcano, the NASA team conducted another simulated Mars landing in 2015 at the Craters of the Moon National Monument in Idaho.
The BASALT team hopes to return to Hawaiʻi in 2017 to repeat the mission in another area of Kīlauea to further refine their planning for eventual exploration of Mars.
The above story is from the USGS Hawaii Volcano Observatory Watch publication at https://hvo.wr.usgs.gov/volcanowatch/view.php?id=479