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By NASA
Curiosity Navigation Curiosity Home Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Images Videos Audio More Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions The Solar System The Sun Mercury Venus Earth The Moon Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets Asteroids, Comets & Meteors The Kuiper Belt The Oort Cloud 3 min read
Sols 4300-4301: Rippled Pages
NASA’s Mars rover Curiosity prepares for a thorough examination of the unusual, dark “Tungsten Hills” rocks in front of it, studying these rugged boulders covered in paper-thin sedimentary layers, some of which contain intriguing ripple structures that may have formed in running water or windblown sand. This image was taken by Left Navigation Camera aboard Curiosity on Sol 4298 — Martian day 4,298 of the Mars Science Laboratory mission — on Sept. 8, 2024, at 06:35:57 UTC. NASA/JPL-Caltech Earth planning date: Monday, Sept. 9, 2024
With today’s plan, Curiosity completes its most southerly planned exploration of the Gediz Vallis channel. From here, our rover will head north and climb out of the channel to explore terrain to the west. Our planned drive to the “Tungsten Hills” rocks, named for a famous mining district near Bishop, California, completed successfully over the weekend, placing a pile of unusual dark rocks within our workspace. Curiosity is currently in the “Bishop” quadrangle on our map, so all targets in this area of Mount Sharp are named after places in the Sierra Nevada and Owens Valley of California. On sols 4300-4301, Curiosity will perform a thorough examination of these rugged boulders, which are covered in paper-thin sedimentary layers like the pages of a book (see image). Some layers have intriguing ripple structures that may have formed in running water or windblown sand. These features are the prime targets for contact science and remote observation at this location.
On Sol 4300, Curiosity will obtain ChemCam laser spectra and Mastcam imagery on a part of the closest plate-like rock called “Bonita Flat,” after a high valley above the southern Kern River canyon in Sequoia National Forest. ChemCam will also obtain telescopic views of a section of the Gediz Vallis channel banks with its RMI camera. Mastcam will take a mosaic of the upper reaches of the channel, then turn its cameras on the interesting bedrock of “Coffeepot Canyon,” honoring a ravine along the precipitous East Fork of the Kaweah River canyon in Sequoia National Park, unfortunately now engulfed in a huge wildfire.
The first science block ends with atmospheric observations, including a dust-devil movie, supra-horizon cloud imaging, and Mastcam measurement of dust in the air across the crater. Curiosity will then use its arm to brush the dust from the closest block in an area dubbed “Pond Lily Lake,” for a petite meadow lake atop the canyon wall of the San Joaquin River, downstream of Devil’s Postpile National Monument. This cleared spot will then be imaged by MAHLI and Mastcam, and its composition will be measured by APXS spectroscopy. MAHLI will perform an intricate “dog’s eye” maneuver to obtain detailed images of ripples in “Window Cliffs,” named after sheer walls above the spectacular fault-controlled Kern River canyon west of 14,505-foot Mount Whitney, the tallest peak in the lower 48 states. MAHLI wraps up a very full day of work by imaging the scalloped edge of the largest nearby block, dubbed “Boneyard Meadow” for a wetland in the western Sierra foothills where many sheep sadly perished due to a late spring snowstorm in 1877.
Early on sol 4301, Curiosity will use Mastcam to thoroughly document the Tungsten Hills in pre-sunrise morning light. Later in the day, a second science block starts with ChemCam spectroscopy and Mastcam imagery of “Castle Domes,” honoring the granite domes of Castle Valley, acclaimed as some of the most beautiful mountain scenery in Kings Canyon National Park. ChemCam RMI will perform telescopic observations of the channel floor. Mastcam will look for possible sulfur rocks at the base of the Tungsten Hills blocks in a target named “Hummingbird Lake,” for an alpine lake at 10,000 feet between Bloody and Lundy Canyons near Mono Lake. This science block of the plan ends with Navcam deck monitoring, dust measurement, and a large dust-devil survey. Curiosity will then drive north, taking a MARDI “sidewalk” video of the terrain under the rover during the drive.
Written by Deborah Padgett, OPGS Task Lead at NASA’s Jet Propulsion Laboratory
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Last Updated Sep 10, 2024 Related Terms
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By NASA
Curiosity Navigation Curiosity Home Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Images Videos Audio More Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions The Solar System The Sun Mercury Venus Earth The Moon Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets Asteroids, Comets & Meteors The Kuiper Belt The Oort Cloud 2 min read
Sols 4297-4299: This Way to Tungsten Hills
This image was taken by Left Navigation Camera aboard NASA’s Mars rover Curiosity on Sol 4296 — Martian day 4,296 of the Mars Science Laboratory mission — on Sept. 6, 2024, at 06:47:03 UTC. NASA/JPL-Caltech Earth planning date: Friday, Sept. 6, 2024
Contact science in our immediate workspace includes a joint effort by MAHLI and APXS to characterize a gray rock with two targets named “Big Baldy” and “Big Bird Lake.” ChemCam focused its Laser Induced Breakdown Spectroscopy (LIBS) instrument on a rock with a reddish coating, “Purple Creek,” and a light-toned rock, “Garlic Meadow,” to determine their chemical composition. ChemCam included a long distance RMI image of the yardang unit that caps Mount Sharp as well as a standard post-drive AEGIS activity, which allows autonomous target selection for upcoming geochemical spectrometry.
The Mastcam team assembled several beautiful mosaics to document Curiosity’s surroundings. One mosaic will extend the imaging of the current workspace and is planned at dusk to take advantage of the diffuse lighting. Two separate mosaics, one of which is in stereo, will characterize the floor of the depression in front of Tungsten Hills to investigate the exposed light rocks and document depositional processes. Finally, a stereo mosaic will image Tungsten Hills and the surrounding terrain in advance of our approach over the weekend.
With the weekend plan in place the science team will now patiently wait for data to be returned and for planning to resume on Monday!
Curiosity completed an impressive 60-meter drive (about 197 feet) across the channel floor within Gediz Vallis and parked along the edge of a shallow linear depression. Just about 20 meters (66 feet) away, an intriguing dark, textured rock named “Tungsten Hills” is the destination for our weekend drive and our contact science on Monday. Today I served as the “Keeper of the Plan” for the Geology theme group and worked with the science team to compile a variety of contact science and targeted science in this three-sol plan.
Written by Sharon Wilson Purdy, Planetary Geologist at the Smithsonian National Air and Space Museum
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By NASA
Curiosity Navigation Curiosity Home Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Images Videos Audio More Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions The Solar System The Sun Mercury Venus Earth The Moon Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets Asteroids, Comets & Meteors The Kuiper Belt The Oort Cloud 2 min read
Sols 4295-4296: A Martian Moon and Planet Earth
Using an onboard focusing process, the Mars Hand Lens Imager (MAHLI) aboard NASA’s Mars rover Curiosity created this product by merging two to eight images previously taken by the MAHLI, which is located on the turret at the end of the rover’s robotic arm. Curiosity performed the merge on Sept. 4, 2024, at 06:30:48 UTC — sol 4294, or Martian day 4,294 of the Mars Science Laboratory mission. The onboard focus merge is sometimes performed on images acquired the same sol as the merge, and sometimes using pictures obtained earlier. Focus merging is a method to make a composite of images of the same target acquired at different focus positions to bring as many features as possible into focus in a single image. The MAHLI focus merge also serves as a means to reduce the number of images sent back to Earth. Each focus merge produces two images: a color, best-focus product and a black-and-white image that scientists can use to estimate focus position for each element of the best-focus product. So up to eight images can be merged, but the number of images returned to Earth is two. NASA/JPL-Caltech/MSSS Earth planning date: Wednesday, Sept. 4, 2024
Today’s two-sol plan contains the usual science blocks filled with contact science and remote science to observe and assess the geology surrounding us. However, the Mastcam team is hoping to capture a special celestial event above the Martian skyline as one of Mars’ moons, Phobos, will be in conjunction with Earth on the evening of the first sol of this plan. So everyone look up, and smile for the camera!
Coming back to our beautiful workspace, in this plan there is a focus on targeting the different colors and tones we can see in the bedrock with our suite of instruments. In the image above we can see some of these varying tones — including gray areas, lighter-toned areas, and areas of tan-colored bedrock — with an image from the MAHLI instrument, Curiosity’s onboard hand lens.
APXS is targeting “Campfire Lake,” a lighter-toned area, and “Gemini,” a more gray-toned area situated in front of the rover. MAHLI is taking a suite of close-up images of these targets too. ChemCam is then taking two LIBS measurements of “Crazy Lake” and “Foolish Lake,” both of which appear to have lighter tones. Mastcam is documenting this whole area with a workspace mosaic and an 8×2 mosaic of “Picture Puzzle,” named after the rock in the image above that was taken during the previous plan. Mastcam will also be capturing a 6×3 mosaic of an outcrop named “Outguard Spire” that has an interesting gray rim. Looking further afield, ChemCam has planned a long-distance RMI image of the yardang unit and Navcam is taking a suprahorizon movie and dust-devil survey for our continued observations of the atmosphere to round out this plan.
Written by Emma Harris, Graduate Student at Natural History Museum, London
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By NASA
Curiosity Navigation Curiosity Home Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Images Videos Audio More Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions The Solar System The Sun Mercury Venus Earth The Moon Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets Asteroids, Comets & Meteors The Kuiper Belt The Oort Cloud 3 min read
Sols 4291-4293: Fairview Dome, the Sequel
This image was taken by Left Navigation Camera aboard NASA’s Mars rover Curiosity on sol 4289 — Martian day 4,289 of the Mars Science Laboratory mission — on Aug. 30, 2024 at 03:48:38 UTC. To the left of the crescent-shaped formation in the low-center part of the image, a wheel track is visible along with an “intriguing” batch of shattered rock where Curiosity had previously driven. NASA/JPL-Caltech Earth planning date: Friday, Aug. 30, 2024
Our backwards drive to “McDonald Pass” got hung up on the steep slopes of “Fairview Dome,” but unlike a lot of movie sequels, our inadvertent return visit to Fairview Dome was at least as good as the original. We took full advantage of the chance to investigate this bedrock rise within Gediz Vallis with multiple contact and remote science targets.
MAHLI and APXS paired up on two different DRT targets of more- and less-nodular spots of bedrock at “Lower Boy Scout Lake” and “Upper Boy Scout Lake.” You can see in the Navcam image above that just beyond the bedrock slab we stopped on, there is a wheel track and a shattered batch of rock. We crushed that bit of rock as we drove backward and were left with a great view of it, including some intriguing bright rock interiors. ChemCam targeted one of those bright rock faces at “North Palisade” and Mastcam acquired a mosaic across the whole field of broken rocks at “Ritter-Banner Saddle.” The churned-up sand of Ritter-Banner Saddle also made for a convenient change detection target as we keep our eye on the wind effects of a potential dust storm rising on Mars. ChemCam had two other opportunities for LIBS analyses at a nodular bedrock target called “Regulation Peak,” and another intriguing vertical rock face with strong color differences called “Simmons Peak.” ChemCam used RMI mosaics to image a collection of higher albedo rocks in Gediz Vallis at a site called “Buckeye Ridge.” Mastcam planned a mosaic of a different part of Gediz Vallis that is in the direction we are driving next, which will help plot those drives and also give us some insight into the boulders strewn about that part of the valley. Closer to the rover, the “Outguard Spire” target was of interest for Mastcam imaging because of its color zonation — the way colors are distributed across different areas, or zones, of the rock. It’s the kind of zonation we intend to study at McDonald Pass. The trough of sand at the “Whitney-Russell Pass” target was of interest for its potential insights into how bedrock blocks break up on Mars.
Monitoring the potential rise of a dust storm meant that the plan was busy with environmental observations. ChemCam acquired a passive sky observation, Navcam collected two rounds of dust-devil imaging, cloud movies, and atmospheric dust measurements, Mastcam acquired multiple atmospheric dust measurements, and REMS ran in longer blocks throughout each sol than it does in normal weather conditions. Dust or not, RAD and DAN passive were planned regularly through the three sols of the plan.
Written by Michelle Minitti, Planetary Geologist at Framework
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By NASA
Lunar geologist Zachary Morse scrabbles over Earth’s rocky landscapes to test equipment for future missions to the Moon and Mars.
Name: Zachary Morse
Title: Assistant Research Scientist in Planetary Geology
Organization: The Planetary Geology, Geophysics and Geochemistry Laboratory, Science Directorate (Code 698)
Zachary Morse is an assistant research scientist in planetary geology at NASA’s Goddard Space Flight Center in Greenbelt, Md. Photo courtesy of Zachary Morse What do you do and what is most interesting about your role here at Goddard? How do you help support Goddard’s mission?
I work with teams that integrate field instrumentation into future lunar and Mars exploration missions. We go to analog field sites, places on Earth that are geologically similar to the Moon or Mars, to test field instruments. I also support the development of science operations for crewed exploration of the lunar surface.
Why did you become a geologist? What is your educational background?
I always knew that I wanted to study space. In college I started in engineering, but switched to geology because much of the science NASA does on the Moon or Mars involves studying the rocks.
In 2013, I got a B.S. in geology from West Virginia University. In 2018, I got a Ph.D. in planetary science from Western University in London, Ontario.
“I work with teams that integrate field instrumentation into future lunar and Mars exploration missions,” said Zachary. “We go to analog field sites, places on Earth that are geologically similar to the Moon or Mars, to test field instruments.”Photo courtesy of Zachary Morse What brought you to Goddard?
In January 2020, I came to Goddard to do a post-doctoral fellowship because I wanted to work on the Remote, In Situ, and Synchrotron Studies for Science and Exploration 2 (Rise2) project. We go into the field to test handheld geologic instruments that could later be incorporated into missions.
What have been some of your favorite trips into the field?
Iceland, Hawaii, and the New Mexico desert, which is our primary field site for Rise2. These were organized as part of the Goddard Instrument Field Team, a group that hosts trips each year to different analog field sites.
The Iceland trip was my favorite because the place we got to explore looked almost exactly like pictures of the Moon’s surface. It was beautiful and the right setting to learn about the Earth and the Moon. Our team was about 40 people. We were there for two weeks. We mostly camped.
It was definitely a unique experience, one hard to put in words. On Earth, you would normally go camping in a lush forest. But there were no trees, just rock and dust. It was absolutely beautiful in its own way.
The Hawaii trip was also unique. Our team of about 30 people spent almost the entire 10 days in the lava tubes. Not many people get to go into lava tubes. It was very exciting. The biggest part of the lava tube was about 20 feet high and about 10 feet wide. The smallest was so small we had to crawl through.
How do you document field work?
In addition to scientific data, we always take pictures of the rocks and outcrops. It is important to document what a site is like before people interact with it. Sometimes we collect rock samples to bring back to the lab, but we leave the place as we found it.
“I always knew that I wanted to study space,” said Zachary. “In college I started in engineering, but switched to geology because much of the science NASA does on the Moon or Mars involves studying the rocks.”Photo courtesy of Zachary Morse Where do you see yourself in five years?
I hope to remain at Goddard; I love it. The team is great and the science is fascinating and important. I want to keep pursuing opportunities for field work. My main goal is to get involved in a lunar mission and support Artemis lunar exploration.
What do you do for fun?
I love the outdoors. I love kayaking on lakes, rivers, and streams. My favorite place is in the Adirondacks. I also love hiking, which I do all over, especially in West Virginia.
Who is your mentor and what did your mentor teach you?
Kelsey Young is my supervisor and mentor. She has taught me so many things including how missions will function and how we can best test equipment in the field for future missions. She taught me how to be organized and focused.
Kelsey Young Dives Into Fieldwork With Aplomb Who inspires you?
Jack Schmitt is an Apollo 17 astronaut who inspired me because he is a geologist. He was the first and only professional geologist who walked on the surface of the Moon during the Apollo missions. I have heard him speak many times and have personally met him.
I would jump at the chance to be the next geologist-astronaut!
What rock formations in the world would you like to explore?
Top of my list would be to explore Acadia National Park in Maine. There is a ton of diverse geology in a small area and the pictures all look stunning. I would also love to visit Glacier National Park to experience the glacier before it melts.
What is your “six-word memoir”? A six-word memoir describes something in just six words.
Exploring Earth to prepare lunar missions.
By Elizabeth M. Jarrell
NASA’s Goddard Space Flight Center, Greenbelt, Md.
Conversations With Goddard is a collection of Q&A profiles highlighting the breadth and depth of NASA’s Goddard Space Flight Center’s talented and diverse workforce. The Conversations have been published twice a month on average since May 2011. Read past editions on Goddard’s “Our People” webpage.
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Last Updated Sep 03, 2024 EditorMadison OlsonContactRob Garnerrob.garner@nasa.govLocationGoddard Space Flight Center Related Terms
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