Members Can Post Anonymously On This Site
Sols 4234-4235: And That’s (Nearly) a Wrap on Mammoth Lakes!
-
Similar Topics
-
By NASA
Curiosity Navigation Curiosity Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Mars Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions All Planets Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets 5 min read
Sols 4232-4233: Going For a Ride, Anyone?
This image shows some of the sand ripples we spot all around the rover between the rocks. It was taken by Mast Camera (Mastcam) onboard NASA’s Mars rover Curiosity on Sol 4225 (2024-06-25 01:10:39 UTC). Earth planning date: Monday, July 1, 2024
Have you ever wondered what it might look like to ride along with the rover? Probably not as much as we have here on the planning team, where we are looking at the images on a daily basis. I always wish I could walk around there myself, or drive around in a vehicle, maybe. As you likely know, we don’t even get video, “just” images. But of course those images are stunning and the landscape is unique and – apart from being scientifically interesting – so very, very beautiful. And some cameras record images so often that it’s actually possible to create the impression of a movie. The front hazard camera is among them. And that can create a stunning impression of looking out of the front window! If you want to see that for yourself, you can! If you go to the NASA interactive tool called “Eyes on the Solar System” there is a Curiosity Rover feature that allows you to do just that: simulate a drive between waypoints and look out of the window, which is the front hazard camera. Here is the link to “Experience Curiosity.” The drive there is a while back, but the landscape is just so fascinating, I can watch and rewatch that any number of times!
Now, after reminiscing about the past, what did we do today? First of all: change all plans we ever had. We don’t have – as scheduled – the SAM data on Earth just yet. But we have a good portion of the sample still in the drill, and if SAM gets their data and wants to do more analysis with that sample, then we can’t move the arm as we originally had planned. Why didn’t we consider that to begin with? Normally, there isn’t enough sample for all the analysis; you may have seen this blog post: “Sols 4118-4119: Can I Have a Second Serving, Please? Oh, Me Too!” But it’s the sample that dictates how much we get to begin with, and how much we need, which only becomes clear as the data come in. And there is an unusually lucky combination here that would avoid us having to drill a second hole for getting the second helping. Instead, we just sit here carefully holding the arm still so we do not lose sample. That saves a lot of rover resources. But then, once we had settled how we adjust to keeping our current position, we also learnt that the uplink time might shift from the original slot we had been allocated to a later one… And all of this with a pretty new-to-the-role Science Operations Working Group (SOWG) chair (me) and a similarly new Geology and Mineralogy theme group science lead. Well, we managed, with lots of help from the great team around us.
Those sudden-change planning days are so tricky because there is so much more to remember. It’s not, “This is what we came to do…,” and it had been carefully pre-planned, and it is all in the notes. Instead, the pre-planning preparation doesn’t fit the new reality anymore, and all that work has to be redone. So we have to do all the pre-planning work, and the actual planning work, and sometimes also account for some “if… then…” scenarios in the same amount of time we usually have to do the planning on the basis of all the pre-planning work.
Sounds stressful? Yes, I can tell you it is!
Once we had changed all the skeleton plans, the team got very excited about the extra time. This is such an interesting area, there are rocks that are almost white, there are darker rocks, very interesting sand features with beautiful ripples, so much to look at! Mars has much to offer here, so the team got to work swiftly and the plan filled up with a great set of observations. ChemCam used LIBS on the target “Tower Peak,” which is one of those white-ish rocks, and on “Quarry Peak.” Mastcam delivers all the pictures to go along with these two activities and gets its own science, too. These are mainly so-called “change detection” images, where the same area is pictured repeatedly to see what particles might move in the time between the two images. ChemCam uses its long-distance imaging capability to add to the stunning images they are getting from faraway rocks. They have two mosaics on a target called “Edge Bench.” There is also a lot of atmospheric science in the plan; looking for dust devils and the opacity of the atmosphere are just two examples. REMS and DAN are also active throughout, to assess the wind, and the water underground, respectively. And as if that weren’t enough, CheMin also performs another night of analysis. We get to uplink a full plan, and we’ll see what the data say and what decisions we’ll make for next Wednesday.
Written by Susanne Schwenzer, Planetary Geologist at The Open University
Share
Details
Last Updated Jul 02, 2024 Related Terms
Blogs Explore More
2 min read Sols 4229-4231: More Analyses of the Mammoth Lakes 2 Sample!
Article
11 hours ago
2 min read Sols 4226-4228: A Powerful Balancing Act
Article
4 days ago
2 min read Interesting Rock Textures Galore at Bright Angel
Article
4 days ago
Keep Exploring Discover More Topics From NASA
Mars
Mars is no place for the faint-hearted. It’s dry, rocky, and bitter cold. The fourth planet from the Sun, Mars…
All Mars Resources
Rover Basics
Mars Exploration Science Goals
View the full article
-
By NASA
Curiosity Navigation Curiosity Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Mars Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions All Planets Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets 2 min read
Sols 4229-4231: More Analyses of the Mammoth Lakes 2 Sample!
The inlet into to the SAM instrument open and awaiting sample delivery. This image was taken by Right Navigation Camera onboard NASA’s Mars rover Curiosity on Sol 4226 (2024-06-26 11:06:46 UTC). Earth Planning Date: Friday, June 28, 2024
After reviewing results from the Evolved Gas Analysis (EGA) experiment that were downlinked yesterday afternoon (Sols 4226-4228: A Powerful Balancing Act), the SAM team decided they’d like to go ahead with a second experiment to analyze the Mammoth Lakes 2 drilled sample. This experiment is known as the Gas Chromatograph/Mass Spectrometer (GCMS) experiment.
SAM, whose full name is Sample Analysis at Mars, is actually a suite of three different analytical instruments that are used to measure the composition of gases which come off drilled samples as we bake them in SAM’s ovens. The three analytical instruments are called a gas chromatograph, quadrupole mass spectrometer, and tunable laser spectrometer. Each one is particularly suited for measuring specific kinds of compounds in the gases, and these include things like water, methane, carbon, or organic (carbon-containing) molecules. In the EGA experiment that we ran in our last plan, we baked the Mammoth Lakes 2 sample and measured the gas compositions using the tunable laser spectrometer and quadrupole mass spectrometer. In this plan, we’ll deliver a new pinch of sample to the SAM oven and then measure the composition of the gases that are released using the gas chromatograph and quadrupole mass spectrometer. By running both experiments, we’ll have a more thorough understanding of the materials that are in this rock.
The SAM GCMS experiment takes a lot of power to run, so it will be the focus of today’s three-sol plan. However, we still managed to fit in some other science activities around the experiment, including a ChemCam RMI mosaic of some far-off ridges, a ChemCam LIBS observation of a nodular target named “Trail Lakes,” environmental monitoring activities, and a couple Mastcam mosaics to continue imaging the terrain around the rover. Should be another fun weekend of science in Gale crater!
Written by Abigail Fraeman, Planetary Geologist at NASA’s Jet Propulsion Laboratory
Share
Details
Last Updated Jul 01, 2024 Related Terms
Blogs Explore More
2 min read Sols 4226-4228: A Powerful Balancing Act
Article
4 days ago
2 min read Interesting Rock Textures Galore at Bright Angel
Article
4 days ago
2 min read Sol 4225: Sliding Down Horsetail Falls
Article
6 days ago
Keep Exploring Discover More Topics From NASA
Mars
Mars is no place for the faint-hearted. It’s dry, rocky, and bitter cold. The fourth planet from the Sun, Mars…
All Mars Resources
Rover Basics
Mars Exploration Science Goals
View the full article
-
By NASA
Curiosity Navigation Curiosity Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Mars Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions All Planets Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets 2 min read
Sols 4226-4228: A Powerful Balancing Act
NASA’s Mars rover Curiosity acquired this image about 10 inches (25 centimeters) from the “Loch Leven” target using its Mars Hand Lens Imager (MAHLI) close-up camera, located on the turret at the end of the rover’s robotic arm, in daylight on June 16, 2024, sol 4216 (or Martian day 4,216) of the Mars Science Laboratory Mission, at 05:12:12 UTC. Earth planning date: Tuesday, June 25, 2024
As documented in a previous blog last week, we continue to juggle power constraints as we focus on analyzing our newest drilled sample on Mars: “Mammoth Lakes 2.” Today, the star of the show is a planned dropoff to SAM (Sample Analysis at Mars instrument suite) and evolved gas analysis of the drill sample. This activity requires significant power so the team had to be judicious in planning other science observations and balancing the power needs of the different activities.
While the team eagerly awaits the outcome of the SAM and CheMin (Chemistry and Mineralogy X-Ray Diffraction instrument) analyses of Mammoth Lakes 2, we continue to acquire other observations in this fascinating area that will assist in our interpretations of the mineralogical data. ChemCam (the Chemistry and Camera instrument) will fire its laser at the “Loch Leven” target to get more chemical data on a target that was previously analyzed by APXS (the Alpha Particle X-Ray Spectrometer). “Loch Leven” is an example of gray material that rims the Mammoth Lakes drill block. The remote imaging capabilities of the ChemCam instrument will also be utilized to acquire a mosaic of a nearby area with interesting lighter- and darker-toned patches within the exposed rocks. Mastcam (Mast camera, for color stills and video) will document the ChemCam “Loch Leven” target and image the Mammoth Lakes 2 drill hole and surrounding fines to monitor any changes resulting from wind. We will also acquire extensions to two previous Mastcam mosaics: “Camp Four” and “Falls Ridge.”
To continue monitoring atmospheric conditions, the team also planned a Navcam (grayscale, stereoscopic Navigation cameras) large dust devil survey and Mastcam tau observation, an overhead image to measure dust in the atmosphere above Curiosity. Standard DAN (Dynamic Albedo of Neutrons instrument), REMS (Rover Environmental Monitoring Station), and RAD (Radiation Assessment Detector) activities round out the plan.
Written by Lucy Thompson, Planetary Geologist at University of New Brunswick
Share
Details
Last Updated Jun 27, 2024 Related Terms
Blogs Explore More
2 min read Interesting Rock Textures Galore at Bright Angel
Article
48 mins ago
2 min read Sol 4225: Sliding Down Horsetail Falls
Article
2 days ago
3 min read Sols 4222-4224: A Particularly Prickly Power Puzzle
Article
6 days ago
Keep Exploring Discover More Topics From NASA
Mars
Mars is no place for the faint-hearted. It’s dry, rocky, and bitter cold. The fourth planet from the Sun, Mars…
All Mars Resources
Rover Basics
Mars Exploration Science Goals
View the full article
-
By NASA
6 min read
Preparations for Next Moonwalk Simulations Underway (and Underwater)
The JunoCam instrument aboard NASA’s Juno spacecraft captured two volcanic plumes rising above the horizon of Jupiter’s moon Io. The image was taken Feb. 3 from a distance of about 2,400 miles (3,800 kilometers).Image data: NASA/JPL-Caltech/SwRI/MSSS, Image processing by Andrea Luck (CC BY) Infrared imagery from the solar-powered spacecraft heats up the discussion on the inner workings of Jupiter’s hottest moon.
New findings from NASA’s Juno probe provide a fuller picture of how widespread the lava lakes are on Jupiter’s moon Io and include first-time insights into the volcanic processes at work there. These results come courtesy of Juno’s Jovian Infrared Auroral Mapper (JIRAM) instrument, contributed by the Italian Space Agency, which “sees” in infrared light. Researchers published a paper on Juno’s most recent volcanic discoveries on June 20 in the journal Nature Communications Earth and Environment.
Io has intrigued the astronomers since 1610, when Galileo Galilei first discovered the Jovian moon, which is slightly larger than Earth. Some 369 years later, NASA’s Voyager 1 spacecraft captured a volcanic eruption on the moon. Subsequent missions to Jupiter, with more Io flybys, discovered additional plumes — along with lava lakes. Scientists now believe Io, which is stretched and squeezed like an accordion by neighboring moons and massive Jupiter itself, is the most volcanically active world in the solar system. But while there are many theories on the types of volcanic eruptions across the surface of the moon, little supporting data exists.
In both May and October 2023, Juno flew by Io, coming within about 21,700 miles (35,000 kilometers) and 8,100 miles (13,000 kilometers), respectively. Among Juno’s instruments getting a good look at the beguiling moon was JIRAM.
Infrared data collected Oct. 15, 2023, by the JIRAM instrument aboard NASA’s Juno shows Chors Patera, a lava lake on Jupiter’s moon Io. The team believes the lake is largely covered by a thick, molten crust, with a hot ring around the edges where lava from Io’s interior is directly exposed to space.NASA/JPL-Caltech/SwRI/ASI/INAF/JIRAM/MSSS Designed to capture the infrared light (which is not visible to the human eye) emerging from deep inside Jupiter, JIRAM probes the weather layer down to 30 to 45 miles (50 to 70 kilometers) below the gas giant’s cloud tops. But during Juno’s extended mission, the mission team has also used the instrument to study the moons Io, Europa, Ganymede, and Callisto. The JIRAM Io imagery showed the presence of bright rings surrounding the floors of numerous hot spots.
“The high spatial resolution of JIRAM’s infrared images, combined with the favorable position of Juno during the flybys, revealed that the whole surface of Io is covered by lava lakes contained in caldera-like features,” said Alessandro Mura, a Juno co-investigator from the National Institute for Astrophysics in Rome. “In the region of Io’s surface in which we have the most complete data, we estimate about 3% of it is covered by one of these molten lava lakes.” (A caldera is a large depression formed when a volcano erupts and collapses.)
Fire-Breathing Lakes
JIRAM’s Io flyby data not only highlights the moon’s abundant lava reserves, but also provides a glimpse of what may be going on below the surface. Infrared images of several Io lava lakes show a thin circle of lava at the border, between the central crust that covers most of the lava lake and the lake’s walls. Recycling of melt is implied by the lack of lava flows on and beyond the rim of the lake, indicating that there is a balance between melt that has erupted into the lava lakes and melt that is circulated back into the subsurface system.
This animation is an artist’s concept of Loki Patera, a lava lake on Jupiter’s moon Io, made using data from the JunoCam imager aboard NASA’s Juno spacecraft. With multiple islands in its interior, Loki is a depression filled with magma and rimmed with molten lava. NASA/JPL-Caltech/SwRI/MSSS “We now have an idea of what is the most frequent type of volcanism on Io: enormous lakes of lava where magma goes up and down,” said Mura. “The lava crust is forced to break against the walls of the lake, forming the typical lava ring seen in Hawaiian lava lakes. The walls are likely hundreds of meters high, which explains why magma is generally not observed spilling out of the paterae” — bowl-shaped features created by volcanism — “and moving across the moon’s surface.”
JIRAM data suggests that most of the surface of these Io hot spots is composed of a rocky crust that moves up and down cyclically as one contiguous surface due to the central upwelling of magma. In this hypothesis, because the crust touches the lake’s walls, friction keeps it from sliding, causing it to deform and eventually break, exposing lava just below the surface.
An alternative hypothesis remains in play: Magma is welling up in the middle of the lake, spreading out and forming a crust that sinks along the rim of the lake, exposing lava.
“We are just starting to wade into the JIRAM results from the close flybys of Io in December 2023 and February 2024,” said Scott Bolton, principal investigator for Juno at the Southwest Research Institute in San Antonio. “The observations show fascinating new information on Io’s volcanic processes. Combining these new results with Juno’s longer-term campaign to monitor and map the volcanoes on Io’s never-before-seen north and south poles, JIRAM is turning out to be one of the most valuable tools to learn how this tortured world works.”
Juno executed its 62nd flyby of Jupiter — which included an Io flyby at an altitude of about 18,175 miles (29,250 kilometers) — on June 13. The 63rd flyby of the gas giant is scheduled for July 16.
More About the Mission
NASA’s Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the Juno mission for the principal investigator, Scott Bolton, of the Southwest Research Institute in San Antonio. Juno is part of NASA’s New Frontiers Program, which is managed at NASA’s Marshall Space Flight Center in Huntsville, Alabama, for the agency’s Science Mission Directorate in Washington. The Italian Space Agency (ASI) funded the Jovian InfraRed Auroral Mapper. Lockheed Martin Space in Denver built and operates the spacecraft.
More information about Juno is available at:
https://science.nasa.gov/mission/juno
News Media Contacts
DC Agle
Jet Propulsion Laboratory, Pasadena, Calif.
818-393-9011
agle@jpl.nasa.gov
Karen Fox / Charles Blue
NASA Headquarters
202-385-1287 / 202-802-5345
karen.c.fox@nasa.gov / charles.e.blue@nasa.gov
Deb Schmid
Southwest Research Institute, San Antonio
210-522-2254dschmid@swri.org
Share
Details
Last Updated Jun 26, 2024 Related Terms
Juno Jet Propulsion Laboratory Jupiter Jupiter Moons Explore More
5 min read Why Scientists Are Intrigued by Air in NASA’s Mars Sample Tubes
Article 6 days ago 2 min read Voyager 1 Returning Science Data From All Four Instruments
The spacecraft has resumed gathering information about interstellar space. NASA’s Voyager 1 spacecraft is conducting…
Article 2 weeks ago 4 min read NASA Announces New System to Aid Disaster Response
In early May, widespread flooding and landslides occurred in the Brazilian state of Rio Grande…
Article 2 weeks ago Keep Exploring Discover Related Topics
Missions
Humans in Space
Climate Change
Solar System
View the full article
-
By NASA
Curiosity Navigation Curiosity Mission Overview Where is Curiosity? Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Mars Resources Mars Missions Mars Sample Return Mars Perseverance Rover Mars Curiosity Rover MAVEN Mars Reconnaissance Orbiter Mars Odyssey More Mars Missions All Planets Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Pluto & Dwarf Planets 3 min read
Sols 4222-4224: A Particularly Prickly Power Puzzle
This image was taken by Mast Camera (Mastcam) onboard NASA’s Mars rover Curiosity on Sol 4219 (2024-06-19 02:22:26 UTC). Earth planning date: Friday, June 21, 2024
All our patient waiting has been rewarded, as we were greeted with the news that our drill attempt of “Mammoth Lakes 2” was successful! You can see the drill hole in the image above, as well as the first place we attempted just to the left. The actual drilling is only the beginning – we want to see what it is we’ve drilled. We’re starting that process this weekend by using our laser spectrometer (LIBS) to check out the drill hole before delivering some of the drilled material to CheMin (the Chemistry & Mineralogy X-Ray Diffraction instrument) to do its own investigations.
The next step in a drill campaign is usually to continue the analysis with SAM (the Sample Analysis at Mars instrument suite), which tends to be quite power hungry. As a result, we want to make sure we’re going into the next plan with enough power for that. That meant that even though we’ve got a lot of free time this weekend, with three sols and CheMin taking up only the first overnight, we needed to think carefully about how we used that free time. Sometimes, when the science teams deliver our plans, we’re overly optimistic. At times this optimism is rewarded, and we’re allowed to keep the extra science in the plan. Today we needed to strategize a bit more, and the midday science operations working group meeting (or SOWG, as it’s known) turned into a puzzle session, as we figured out what could move around and what we had to put aside for the time being.
An unusual feature of this weekend’s plan was a series of short change-detection observations on “Walker Lake” and “Finch Lake,” targets we’ve looked at in past plans to see wind-driven movement of the Martian sand. These were peppered through the three sols of the plan, to see any changes during the course of a single sol. While these are relatively short observations – only a few minutes – we do have to wake the rover to take them, which eats into our power. Luckily, the science team had considered this, and classified the observations as high, middle, or low priority. This made it easy to take out the ones that were less important, to save a bit of power.
Another power-saving strategy is considering carefully where observations go. A weekend plan almost always includes an “AM ENV Science Block” – dedicated time for morning observations of the environment and atmosphere. Usually, this block goes on the final sol of the plan, but we already had to wake up the morning of the first sol for CheMin to finish up its analysis. This meant we could move the morning ENV block to the first sol, and Curiosity got a bit more time to sleep in, at the end of the plan.
Making changes like these meant not only that we were able to finish up the plan with enough power for Monday’s activities, but we were still able to fit in plenty of remote science. This included a number of mosaics from both Mastcam and ChemCam on past targets such as “Whitebark Pass” and “Quarry Peak.” We also had two new LIBS targets: “Broken Finger Peak” and “Shout of Relief Pass.” Aside from our morning block, ENV was able to sneak in a few more observations: a dust-devil movie, and a line-of-sight and tau to keep an eye on the changing dust levels in the atmosphere.
Written by Alex Innanen, Atmospheric Scientist at York University
Share
Details
Last Updated Jun 21, 2024 Related Terms
Blogs Explore More
2 min read A Bright New Abrasion
Last week, Perseverance arrived at the long-awaited site of Bright Angel, named for being a…
Article
1 day ago
6 min read Sols 4219-4221: It’s a Complex Morning…
Article
3 days ago
2 min read Perseverance Finds Popcorn on Planet Mars
After months of driving, Perseverance has finally arrived at ‘Bright Angel’, discovering oddly textured rock…
Article
3 days ago
Keep Exploring Discover More Topics From NASA
Mars
Mars is no place for the faint-hearted. It’s dry, rocky, and bitter cold. The fourth planet from the Sun, Mars…
All Mars Resources
Rover Basics
Mars Exploration Science Goals
View the full article
-
-
Check out these Videos
Recommended Posts
Join the conversation
You can post now and register later. If you have an account, sign in now to post with your account.