InSight

{{Short description|NASA Mars lander (2018–2022)}}

{{redirect|Insight (spacecraft)|the Chinese spacecraft also called Insight|Hard X-ray Modulation Telescope|other uses|Insight (disambiguation)}}

{{distinguish|iSight}}

{{Use American English|date=December 2021}}

{{Use dmy dates|date=October 2019}}

{{Infobox spaceflight

| name = InSight

| names_list = {{ubl|InSight|GEMS|Discovery 12}}

| image = File:PIA19664-MarsInSightLander-Assembly-20150430.jpg

| image_caption = The InSight lander with solar panels deployed in a cleanroom during preflight testing

| mission_type = Mars lander

| operator = NASA{{\}}JPL

| COSPAR_ID = 2018-042A

| SATCAT = 43457

| website = {{URL|https://science.nasa.gov/mission/insight/|science.nasa.gov}}

| mission_duration = {{ubli|Planned: 709 sols (2 years)| Final: {{age in sols|2018|11|26|2022|12|15}} sols ({{time interval|26 Nov 2018|15 Dec 2022|show=ymd|sep=,}})}}

| manufacturer = Lockheed Martin Space

| launch_mass = {{cvt|694|kg}}

| landing_mass = {{cvt|358|kg}}

| dimensions = {{cvt|6.0|xx|1.56|xx|1.0|m}} (deployed)

| power = 600 watts

| launch_date = 5 May 2018, 11:05:01 UTC

| launch_rocket = {{ubli|Atlas V 401|AV-078}}

| launch_site = Vandenberg, SLC-3E

| launch_contractor = United Launch Alliance

| entered_service = 26 November 2018

| disposal_type = Decommissioned

| declared = 21 December 2022

| last_contact = 15 December 2022 (official){{r|NYT-20221222|nasa20221220}}

| interplanetary = {{Infobox spaceflight/IP

| type = lander

| object = Mars

| arrival_date = 26 November 2018, 19:52:59 UTC
MSD 51511 05:14 AMT

| lost contact = December 18th

| location = Elysium Planitia{{r|landing|insight-selection}}
{{Coord|4.5024|N|135.6234|E|globe:Mars|name=InSight landing site}}

}}

{{Infobox spaceflight/IP

| type = flyby

| object = Mars

| component = Mars Cube One (MarCO)

| arrival_date = 26 November 2018, 19:52:59 UTC

| distance = {{cvt|3500|km}}

}}

| instruments_list = {{Infobox spaceflight/Instruments

| acronym1 = SEIS | name1 = Seismic Experiment for Interior Structure

| acronym2 = HP3 | name2 = Heat Flow and Physical Properties Package

| acronym3 = RISE | name3 = Rotation and Interior Structure Experiment

| acronym4 = TWINS | name4 = Temperature and Winds for InSight

}}

| insignia = InSight Mission Logo.svg

| insignia_caption = InSight mission logo

| insignia_size = 200px

| programme = Discovery Program

| previous_mission = GRAIL

| next_mission = Lucy

| programme2 = Mars Exploration Program

| previous_mission2 = MAVEN

| next_mission2 = Mars 2020

}}

The Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) mission was a robotic lander designed to study the deep interior of the planet Mars.{{r|insight-facts|NYT-20180430|washington1}} It was manufactured by Lockheed Martin Space, was managed by NASA's Jet Propulsion Laboratory (JPL), and two of its three scientific instruments were built by European agencies. InSight confirmed "marsquakes" on the planet and thus a still active interior.

The mission launched on 5 May 2018 at 11:05:01 UTC aboard an Atlas V-401 launch vehicle and successfully landed at Elysium Planitia on Mars on 26 November 2018 at 19:52:59 UTC.{{r|NYT-20181126|guardian1|NYT-20180505|insight-launch}} InSight was active on Mars for {{age in sols|2018|11|26|2022|12|15}} sols ({{age in days|2018|11|26|2022|12|15}} days; {{Age in years and days|26 November 2018|15 December 2022}}).

InSight{{'s}} objectives were to place a seismometer, called Seismic Experiment for Interior Structure (SEIS), on the surface of Mars to measure seismic activity and provide accurate 3D models of the planet's interior; and measure internal heat transfer using a heat probe called HP3 to study Mars's early geological evolution. This was intended to provide a new understanding of how the Solar System's terrestrial planets – Mercury, Venus, Earth, Mars – and Earth's Moon formed and evolved.

The lander was originally planned for launch in March 2016.{{r|washington1|sciam20171114}} An instrument problem delayed the launch beyond the 2016 launch window. NASA officials rescheduled the InSight launch to May 2018 and during the wait the instrument was repaired. This increased the total cost from US$675 million to US$830 million.{{r|nasa20160902|wsj1}}

InSight successfully landed on Mars on 26 November 2018. Due to excessive dust on its solar panels preventing it from recharging, NASA put InSight in low-power mode for detecting seismic events in July 2022 and continued monitoring the lander through the operational period ending in December 2022. On 20 December 2022, NASA announced that the InSight lander had lost communications with Earth on 15 December 2022, with the end of the mission being declared on 21 December 2022.{{r|NYT-20221222|nasa20221220|nasa20221221}}

History

= Discovery Program selection =

File:PIA19666-MarsInSightLander-Assembly-20150429.jpg

InSight was initially known as GEMS (Geophysical Monitoring Station), but its name was changed in early 2012 following a request by NASA. Out of 28 proposals from 2010, it was one of the three Discovery Program finalists receiving $3 million in May 2011 to develop a detailed concept study. In August 2012, InSight was selected for development and launch. Managed by NASA's Jet Propulsion Laboratory (JPL) with participation from scientists from several countries, the mission was cost-capped at US$425 million, not including launch vehicle funding.

By reusing the landing system designed for the Mars Phoenix lander, which successfully landed on Mars in 2008, mission costs and risks were reduced.

= Schedule issues =

Lockheed Martin began construction of the lander on 19 May 2014, with general testing starting on 27 May 2015.

A persistent vacuum leak in the CNES-supplied seismometer known as the Seismic Experiment for Interior Structure (SEIS) led NASA to postpone the planned launch in March 2016 to May 2018. When InSight was delayed, the rest of the spacecraft was returned to Lockheed Martin's factory in Colorado for storage, and the Atlas V launch vehicle intended to launch the spacecraft was reassigned to the WorldView-4 mission.

On 9 March 2016, NASA officials announced that InSight would be delayed until the 2018 launch window at an estimated cost of US$150 million. The spacecraft was rescheduled to launch on 5 May 2018 for a Mars landing on 26 November 2018 at 20:00 UTC. The flight plan remained unchanged with launch using an Atlas V launch vehicle from Vandenberg Space Force Base in California. NASA's Jet Propulsion Laboratory was tasked with redesigning and building a new vacuum enclosure for the SEIS instrument, while CNES conducted instrument integration and testing.

On 22 November 2017, InSight completed testing in a thermal vacuum, also known as TVAC testing, where the spacecraft is put in simulated space conditions with reduced pressure and various thermal loads. On 23 January 2018, after a long storage, its solar panels were once again deployed and tested, and a second silicon chip containing 1.6 million names from the public was added to the lander.

= Effects of Martian dust and end of operations =

The InSight lander, powered by solar panels and batteries, relies on periodic wind gusts called "cleaning events" to reduce dust accumulation on the panels. Elysium Planitia, the landing site of InSight, has experienced fewer cleaning events than needed to keep the science operations powered. In February 2021, at the start of the Martian winter, InSight's solar cells were producing 27% of capacity due to a thick covering of dust on the panels. At that time NASA began the process of putting the lander into hibernation mode, shutting down data-gathering instruments on a schedule to conserve enough power to keep the lander electronics warm through the Martian winter. NASA had hoped that weather conditions would improve and allow InSight to store enough energy to come out of hibernation in July 2021.

In May 2021, some generation capacity was restored by using the arm to position sand so it could blow onto the solar panels and scour them clean.

NASA determined in May 2022 that there was too much dust on the panels to continue the mission. InSight was generating only one-tenth of the power from the sunlight than it did upon arrival. They put the lander in a low-power mode in July 2022 to continue monitoring for seismic events. NASA continued to monitor InSight until the end of 2022, when the spacecraft missed two consecutive communication attempts.

Science background

= Seismic vibrations =

File:PIA25282-MarsInSightLander-InsideMars-20220517.jpg

Both Viking spacecraft carried seismometers mounted on their landers, and in 1976 vibrations were picked up from various lander operations and from the wind. However, the Viking 1 lander's seismometer did not deploy properly and did not unlock; the locked seismometer could not operate.

The Viking 2 seismometer unlocked; it operated and returned data to Earth. One problem was accounting for other data. On Sol 80, the Viking 2 seismometer detected an event. No wind data were recorded at the same time, so it was not possible to determine whether the data indicated a seismic event or wind gust. Other lacking data would have been useful to rule out other sources of vibrations. Two other problems were the location of the lander and that a certain level of wind on Mars caused a loss of sensitivity for the Viking 2 seismometer. To overcome these and other issues, InSight had many other sensors, was placed directly on the surface, and also had a windshield.

Despite the difficulties, the Viking 2 seismometer readings were used to estimate a Martian geological crust thickness between {{convert|8.7|and|11.2|mi|km|0|order=flip|abbr=on}} at the Viking 2 lander site. The Viking 2 seismometer did detect vibrations from Mars winds complementing the meteorology results. There was the aforementioned candidate for a possible marsquake, but it was not particularly definitive. The wind data did prove useful in its own right, and despite the limitations of the data, widespread and large marsquakes were not detected.

Seismometers were also left on the Moon, starting with Apollo 11 in 1969, and also by Apollo 12, 14, 15 and 16 missions and provided many insights into lunar seismology, including the discovery of moonquakes. The Apollo seismic network, which was operated until 1977, detected at least 28 moonquakes up to 5.5 on the Richter scale.

One of the aspects of the InSight mission was to compare the Earth, Moon, and Mars seismic data.{{blockquote|Well, seismic investigation is really the heart of this mission. Seismology is the method that we've used to gain almost everything we know, all the basic information about the interior of the Earth, and we also used it back during the Apollo era to understand and to measure sort of the properties of the inside of the moon. And so, we want to apply the same techniques but use the waves that are generated by Mars quakes, by meteorite impacts to probe deep into the interior of Mars all the way down to its core.|Gravity Assist: Mars and InSight with Bruce Banerdt (3 May 2018)}}

On 4 May 2022, a large marsquake, estimated at magnitude 5, was detected by the seismometer on the InSight lander.

{{multiple images |header=Mars quake detected (4 May 2022) |direction=horizontal|align=center |width= |image1=PIA25044-MarsInSightLander-BigQuake-20220504.jpg |width1=325 |image2=PIA25180-MarsInSightLander-BigQuake-Graph-20220504.jpg |width2=250 |image3=PIA25281-MarsInSightLander-MarsQuake-20220504.webm |caption3= |width3=190 |footer= }}

On 25 October 2023, scientists, helped by information from InSight, reported that the planet Mars has a radioactive magma ocean under its crust.

= Planetary precession =

Radio Doppler measurements were taken with Viking and twenty years later with Mars Pathfinder, and in each case the axis of rotation of Mars was estimated. By combining this data, the core size was constrained, because the change in axis of rotation over 20 years allowed a precession rate and from that the planet's moment of inertia to be estimated. InSight{{'s}} measurements of crust thickness, mantle viscosity, core radius and density, and seismic activity were planned to result in a three- to tenfold increase in accuracy compared to previous data.

Objectives

The InSight mission placed a single stationary lander on Mars to study its deep interior and address a fundamental issue of planetary and Solar System science: understanding the processes that shaped the rocky planets of the inner Solar System (including Earth) more than four billion years ago.

File:Terrestrial Planet Interiors (Earth, Mars and Moon) - Artist's Concept.jpg

InSight{{'s}} primary objective was to study the earliest evolutionary processes that shaped Mars. By studying the size, thickness, density and overall structure of Mars's core, mantle and crust, as well as the rate at which heat escapes from the planet's interior, InSight will provide a glimpse into the evolutionary processes of all of the rocky planets in the inner Solar System. The rocky inner planets share a common ancestry that begins with accretion. As the body increases in size, its interior heats up and evolves to become a terrestrial planet, containing a core, mantle and crust. Despite this common ancestry, each of the terrestrial planets is later shaped and molded through the poorly understood process of differentiation. InSight mission's goal was to improve the understanding of this process and, by extension, terrestrial evolution, by measuring the planetary building blocks shaped by this differentiation: a terrestrial planet's core, mantle and crust.

File:PIA22745-Mars-InSightLander-ArtistConcept-20181030.jpg

The mission will determine if there is any seismic activity, measure the rate of heat flow from the interior, estimate the size of Mars's core and whether the core is liquid or solid. This data would be the first of its kind for Mars. It is also expected that frequent meteor airbursts (10–200 detectable events per year for InSight) will provide additional seismo-acoustic signals to probe the interior of Mars. The mission's secondary objective was to conduct an in-depth study of geophysics, tectonic activity and the effect of meteorite impacts on Mars, which could provide knowledge about such processes on Earth. Measurements of crust thickness, mantle viscosity, core radius and density, and seismic activity should result in a three- to tenfold increase in accuracy compared to current data. This is the first time a robotic lander dug this deep into the martian crust.

In terms of fundamental processes shaping planetary formation, it is thought that Mars contains the most in-depth and accurate historical record, because it is big enough to have undergone the earliest accretion and internal heating processes that shaped the terrestrial planets, but is small enough to have retained signs of those processes. The science phase is expected to last for two years.

In March 2021, NASA reported, based on measurements of over 500 Marsquakes by the InSight lander on the planet Mars, that the core of Mars is between {{convert|1810 and 1860|km|mi|abbr=on}}, about half the size of the core of Earth, and significantly smaller than thought earlier, suggesting a core of lighter elements.

2024 groundwater discovery

{{See also|Groundwater on Mars}}

In August 2024, a reservoir of liquid water was discovered on Mars – deep in the rocky outer crust of the planet. The findings came from a new analysis of data from Nasa’s Mars Insight Lander, which recorded four years' of vibrations – Mars quakes – from deep inside the Red Planet. The analysis revealed reservoirs of water at depths of about six to 12 miles (10 to 20km) in the Martian crust.{{Cite web |title=Mars water: Liquid water reservoirs found under Martian crust |url=https://www.bbc.com/news/articles/czxl849j77ko |access-date=2024-08-16 |website=www.bbc.com |language=en-GB}}{{Cite web |last=Strickland |first=Ashley |date=2024-08-12 |title=Oceans of water may be trapped deep beneath the Martian surface |url=https://edition.cnn.com/2024/08/12/science/mars-crust-water-reservoir-insight/index.html |access-date=2024-08-16 |website=CNN |language=en}}

As per estimates, there may be enough water, trapped in tiny cracks and pores of rock in the middle of the Martian crust, to fill oceans on the planet’s surface. The groundwater would likely cover the entirety of Mars to a depth of 1 mile (1.6 kilometers), the study found.

Design

File:InSight Lander Transparent.png

The mission further develops a design based on the 2008 Phoenix Mars lander. Because InSight is powered by solar panels, it landed near the equator to enable maximum power for a projected lifetime of two years (1 Martian year). The mission includes two relay microsatellites called Mars Cube One (MarCO) that launched with InSight but were flying in formation with InSight to Mars.

Three major aspects to the InSight spacecraft are the cruise stage, the entry, descent, and landing system, and the lander.

= Overall specifications =

;Mass

  • Total mass during cruise: {{convert|694|kg|lb|abbr=on}}
  • Lander: {{convert|358|kg|lb|abbr=on}}
  • Aeroshell: {{convert|189|kg|lb|abbr=on}} Aeroshell Diameter (backshell and heat shield) : 2.64 meters (8.67 ft)
  • Cruise stage: {{convert|79|kg|lb|abbr=on}}
  • Propellant and pressurant: {{convert|67|kg|lb|abbr=on}}
  • Relay probes flew separately but they weighed {{convert|13.5|kg|lb|0|abbr=on}} each (there were 2)

= Lander specifications =

  • Lander mass: {{convert|358|kg|lb|abbr=on}} including about 50 kg of science payload.
  • Mars weight (0.376 of Earth's): {{convert|1320|N|lbf|abbr=on}}
  • About {{convert|6.0|m|ft|abbr=on}} wide with solar panels deployed.
  • The science deck is about {{convert|1.56|m|ft|abbr=on}} wide and between {{convert|0.83|and|1.08|m|ft|abbr=on}} high (depending on leg compression after landing).
  • The length of the robotic arm is {{convert|1.8|m|ft|abbr=on}}
  • Tilt of lander at landing on Mars: 4°

== Power ==

File:PIA22835-MarsProbes-SingleSolGeneratedEnergy-20181130-corrected.png

Power is generated by two round solar panels, each {{convert|2.15|m|ft|abbr=on}} in diameter when unfurled, and consisting of SolAero ZTJ triple-junction solar cells made of InGaP/InGaAs/Ge arranged on Orbital ATK UltraFlex arrays. After touchdown on the Martian surface, the arrays are deployed by opening like a folding fan.{{r|solaero1|atk1}}

  • Rechargeable batteries
  • Solar panels yielded 4.6 kilowatt-hours on Sol 1

= Payload =

File:PIA17358-MarsInSightLander-20140326.jpg

File:HP3 burrowing mechanism.gif

InSight{{'s}} lander payload had a total mass of {{cvt|50|kg}}, including science instruments and support systems such as the Auxiliary Payload Sensor Suite, cameras, the instrument deployment system, and a laser retroreflector.

InSight performed three major experiments using SEIS, HP3 and RISE. SEIS is a very sensitive seismometer, measuring vibrations; HP3 involves a burrowing probe to measure the thermal properties of the subsurface. RISE uses the radio communication equipment on the lander and on Earth to measure the overall movement of planet Mars that could reveal the size and density of its core.

  • The Seismic Experiment for Interior Structure (SEIS) measured marsquakes and other internal activity on Mars, and the response to meteorite impacts, to better understand the planet's history and structure.{{r|nasa20140210|newsci2|Sunil_2016}} SEIS was provided by the French Space Agency (CNES), with the participation of the Institut de Physique du Globe de Paris (IPGP), the Swiss Federal Institute of Technology (ETH), the Max Planck Institute for Solar System Research (MPS), Imperial College, Institut supérieur de l'aéronautique et de l'espace (ISAE) and JPL.{{r|arstech1|Lognonne_2011}} The seismometer can also detect sources including atmospheric waves and tidal forces from Mars's moon Phobos.{{r|Panning_2017|octoberpres}} A leak in SEIS in 2016 had forced a two-year mission postponement. The SEIS instrument is supported by meteorological tools including a vector magnetometer provided by UCLA that measures magnetic disturbances, air temperature, wind speed and wind direction sensors based on the Spanish/Finnish Rover Environmental Monitoring Station; and a barometer from JPL.{{r|space.com12|Banerdt20130307}}
  • The Heat Flow and Physical Properties Package (HP3), provided by the German Aerospace Center (DLR) included a radiometer and a heat flow probe.{{r|octoberpres|nasapr20120820|flow|mtm}} The probe, referred to as a "self-hammering nail" and nicknamed "the mole", was designed to burrow {{convert|5|m|ft|abbr=on}} below the Martian surface while trailing a tether, with embedded heat sensors to study the thermal properties of Mars's interior, and thus reveal unique information about the planet's geologic history.{{r|octoberpres|nasapr20120820|flow|mtm}} The hammering mechanism inside the mole was designed by the Polish company Astronika and the Space Research Centre of the Polish Academy of Sciences under contract and in cooperation with DLR. The tether contains precise temperature sensors every {{convert|10|cm|abbr=on}} to measure the temperature profile of the subsurface.{{r|octoberpres|insight-hp3}}
  • The Rotation and Interior Structure Experiment (RISE) led by the Jet Propulsion Laboratory (JPL), was a radio science experiment that uses the lander's X band radio to provide precise measurements of planetary rotation to better understand the interior of Mars. X band radio tracking, capable of an accuracy under {{cvt|2|cm}}, builds on previous Viking program and Mars Pathfinder data.{{r|octoberpres}} The previous data allowed the core size to be estimated, but with more data from InSight, the nutation amplitude can be determined. Once spin axis direction, precession, and nutation amplitudes are better understood, it should be possible to calculate the size and density of the Martian core and mantle. This should increase the understanding of the formation of terrestrial planets (e.g. Earth) and rocky exoplanets.
  • Temperature and Winds for InSight (TWINS), fabricated by the Spanish Astrobiology Center, monitors weather at the landing site.{{r|bb13|space.com12}}
  • Laser RetroReflector for InSight (LaRRI) is a corner cube retroreflector provided by the Italian Space Agency and mounted on InSight{{'s}} top deck.{{r|Dell'Agnello2017|Banerdt2016}} It enables passive laser range-finding by orbiters after the lander is retired, and will function as a node in a proposed Mars geophysical network. This device previously flew on the Schiaparelli lander as the Instrument for Landing-Roving Laser Retroreflector Investigations (INRRI), and is an aluminum dome {{convert|54|mm|in|1|abbr=on}} in diameter and {{convert|25|g|oz|1|abbr=on}} in mass featuring eight fused silica reflectors.
  • Instrument Deployment Arm (IDA) is a {{cvt|1.8|m|ft}} robotic arm that deployed the SEIS, wind and thermal shield, and HP3 instruments to Mars's surface. It is a 4 DOF motorized manipulator, constructed from carbon-fiber composite tubes. Originally intended for the canceled Mars Surveyor mission, the IDA features a scoop, wax actuated grappling claw, and the IDC camera.{{r|IDA|youtube1}}
  • The Instrument Deployment Camera (IDC) is a color camera based on the Mars Exploration Rover and Mars Science Laboratory navcam design. It is mounted on the Instrument Deployment Arm and images the instruments on the lander's deck and provides stereoscopic views of the terrain surrounding the landing site. It features a 45° field of view and uses a 1024 × 1024 pixel CCD detector. The IDC sensor was originally black and white for best resolution; a program was enacted that tested with a standard Hazcam and, since development deadlines and budgets were met, it was replaced with a color sensor.
  • The Instrument Context Camera (ICC) is a color camera based on the MER/MSL Hazcam design. It is mounted below the lander's deck, and with its wide-angle 120° panoramic field of view provides a complementary view of the instrument deployment area. Like the IDC, it uses a 1024 × 1024 pixel CCD detector.

{{clear}}

{{multiple image

| align = center

| total_width = 800

| caption_align = center

| image1 = PIA19144-MarsMission-InSight-Testing-20150304.jpg

| caption1 = A test of the 2.4 meter long Instrument Deployment Arm, seen deploying SEIS

| image2 = Hp3sol10.jpg

| caption2 = HP3 on the lander deck on Sol 10

| image3 = InSight's HP3 instrument diagram.png

| caption3 = HP3 diagram

| image4 = Twinsboom.jpg

| caption4 = TWINS meteorological sensor

| image5 = LaRRI retroreflector on InSight (PIA22206).png

| caption5 = LaRRI, the laser retroreflector on InSight{{'s}} deck

}}

The two relay 6U cubesats were part of the overall InSight program, and were launched at the same time as the lander but they were attached to the centaur upper stage (InSight's second stage in the launch). They were ejected from the stage after launch and coasted to Mars independent of the main InSight cruise stage with the lander.

= Twin Lander =

JPL also built a full-scale engineering model, named ForeSight. This was used to practice instrument deployment, trial new ways to deploy the HP3 instrument, and test methods to reduce seismometer noise.

With the mission now ended, the testbed is being scrapped and its parts will be offered to other teams such as the Mars Sample Retrieval Lander (SRL) for the Mars Sample Return campaign at JPL to be repurposed for their own needs. Anything that is not needed will go into storage. As of now, no attempt is planned to be undertaken to restore ForeSight or to send it to a museum.

Journey to Mars

= Launch =

On 28 February 2018, InSight was shipped via C-17 cargo aircraft from the Lockheed Martin Space building in Denver to Vandenberg Air Force Base in California in order to be integrated to the launch vehicle. The lander was launched on 5 May 2018 and arrived on Mars at approximately 19:54 UTC on 26 November 2018.

File:Despegue de InSight (VAFB-20180505-PH JBS01 0012).jpg rocket carrying InSight and MarCO from Vandenberg Space Launch Complex 3-E]]

The spacecraft was launched on 5 May 2018 at 11:05 UTC on an Atlas V 401 launch vehicle (AV-078) from Vandenberg Air Force Base Space Launch Complex 3-East. This was the first American interplanetary mission to launch from California.

The launch was managed by NASA's Launch Services Program. InSight was originally scheduled for launch on 4 March 2016 on an Atlas V 401 (4 meter fairing/zero (0) solid rocket boosters/single (1) engine Centaur) from Vandenberg Air Force Base in California, U.S., but was called off in December 2015 due to a vacuum leak on the SEIS instrument.{{r|AP-20151222|NYT-20151222|nasa20151222}} The rescheduled launch window ran from 5 May to 8 June 2018.

Major components of the launch vehicle include:

  • Common Core Booster
  • This launch did not use additional solid rocket boosters
  • Centaur with Relay CubeSats
  • InSight in a Payload fairing

The journey to Mars took 6.5 months across {{convert|301|e6mi|e6km|order=flip|abbr=unit}} for a touchdown on 26 November.{{r|NYT-20180505|insight-launch}} After a successful landing, a three-month-long deployment phase commenced as part of its two-year (a little more than one Martian year) prime mission.{{r|insight-surface|nasa20181121}}

{{clear}}

{{multiple image

| align = center

| total_width = 800

| image1 = SLC-3 Service Tower Rolls Back for InSight.jpg

| caption1 = Service tower rolls back.

| image2 = InSight Prelaunch (NHQ201805050009).jpg

| caption2 = Pre-launch

| image3 = InSight rises above the fog (VAFB-20180505-PH CSH01 0001).jpg

| caption3 = InSight heading to space

}}

{{multiple image|align=center|total_width=500| caption_align=center

|header = InSight on way to Mars

|image1=PIA22547-Mars-InSightLander-ArtistConcept-20180820.jpg|caption1=Exterior (artist concept)

|image3=PIA22647-Mars-InSightLander-InteriorDuringSpaceFlight-20180820.jpg|caption3=Interior

}}

= Cruise =

File:Animation of InSight trajectory.gif}}{{·}}{{legend2| Lime|Mars}}]]

After its launch from Earth on 5 May in 2018, it coasted through interplanetary space for 6.5 months traveling across {{convert|301|e6mi|e6km|order=flip|abbr=unit}} for a touchdown on 26 November in that year.{{r|NYT-20180505|insight-launch}}

InSight cruise stage departed Earth at a speed of {{convert|10000|km/h}}. The MarCo probes were ejected from the 2nd stage Centaur booster and traveled to Mars independent of the InSight cruise stage, but they were all launched together.{{citation needed|date=June 2020}}

During the cruise to Mars, the InSight cruise stage made several course adjustments, and the first of these (TCM-1) took place on 22 May 2018. The cruise stage that carries the lander includes solar panels, antenna, star trackers, Sun sensor, inertial measurement unit among its technologies. The thrusters are actually on the InSight lander itself, but there are cutouts in the shell so the relevant rockets can vent into space.

The final course correction was 25 November 2018, the day before its touch down. A few hours before making contact with the Martian atmosphere, the cruise stage was jettisoned, on 26 November 2018.

= Entry, descent, and landing =

On 26 November 2018, at approximately 19:53 UTC, mission controllers received a signal via the Mars Cube One (MarCO) satellites that the spacecraft had successfully touched down at Elysium Planitia.{{r|NYT-20180505|NYT-20181126|insight-launch}} After landing, the mission took three months to deploy and commission the geophysical science instruments.{{r|insight-surface|nasa20181121}} It then began its mission of observing Mars, which was planned to last for two years.

The spacecraft's mass that entered the atmosphere of Mars was {{convert|1340|lb|kg|0|abbr=on}}. There were three major stages to InSight's landing:

  • Entry: after separating from the cruise stage the aeroshell enters the atmosphere and is subject to air and dust in the Martian atmosphere.
  • Parachute descent: at a certain speed and altitude a parachute is deployed to slow the lander further.
  • Rocket descent: closer to the ground the parachute is ejected and the lander uses rocket engines to slow the lander before touchdown.

Landing sequence:

  • 25 November 2018, final course correction before EDL.
  • 26 November 2018, Cruise stage jettisoned before entering the atmosphere.
  • Several minutes later, the aeroshell containing the lander makes contact with the upper Martian atmosphere at {{cvt|12300|mph}}.
  • At this point it is {{convert|80|miles}} above Mars and in the next few minutes it lands, but undergoes many stages.
  • Aeroshell is heated to {{cvt|1500|C|F}} during descent.
  • At {{cvt|385|m/s}} and ~{{cvt|11100|m}} above the surface, the parachute is deployed.
  • Several seconds later, the heat shield is jettisoned from the lander.
  • The landing legs extended.
  • Landing radar activated.
  • Backshell jettisoned at a speed of about {{cvt|60|m/s}} and at {{cvt|1100|m}} altitude.
  • Landing rockets turned on.
  • Roughly {{cvt|50|m}} from the ground constant velocity mode is entered.
  • Approaches ground at about {{cvt|5|mph}}.
  • Touchdown{{mdash}}each of the three lander legs have a sensor to detect ground contact.
  • Descent rockets are turned off at touchdown.
  • Begin surface operations.

The lander's mass is about {{convert|358|kg|lb|abbr=on}} but on Mars, which has 0.376 of Earth's gravity, it only weighs the equivalent of a {{convert|135|kg|lb|abbr=on}} object on Earth.

{{clear}}

{{further|Mars atmospheric entry|Mars landing|List of artificial objects on Mars}}

{{multiple image

| align = center

| total_width = 1000

| image1 = InSight lander separating from its cruise stage PIA22828.jpg

| caption1 = Illustration of the InSight cruise stage and lander separating prior to landing

| image2 = Insight landing-640x350.gif

| caption2 = Touchdown on Elysium Planitia (animation)

| image3 = PIA22812-Mars-InSightLander-Landing-20181010.jpg

| caption3 = A simulated view of NASA's InSight lander about to land on the surface of Mars

}}

{{Multiple image

| align = center

| direction = horizontal

| width = 400

| image1 = PIA22829 InSight's First Image from Mars, Annotated version.jpg

| image2 = PIA22575 IDC Camera First Image.jpg

| footer = First light on the surface of Mars from the Instrument Context Camera (ICC, left) and the Instrument Deployment Camera (IDC, right)
26 November 2018 (Touch down-day // Sol 0)

}}

{{multiple image

| header = After InSight landing (14 December 2018)

| align = center

| direction = horizontal

| width = 400

| image1 = PIA23301-MarsInSightLander-PitsMadeByThrusters-20181214.jpg

| caption1 = The pits made by thrusters (contrast-enhanced without color-correction)

| width1 =

| image2 = PIA23250-MarsinSightLander-SoilChurnedByThrusters-20181214.jpg

| caption2 = The soil churned by thrusters

| width2 =

| footer =

}}

On 26 November 2018, InSight successfully touched down in Elysium Planitia.

A few hours after landing, NASA's 2001 Mars Odyssey orbiter relayed signals indicating that InSight{{'s}} solar panels had successfully unfurled and are generating enough electrical power to recharge its batteries daily. Odyssey also relayed a pair of images showing InSight{{'s}} landing site. More images were acquired in stereo pairs to create 3D images, allowing InSight to find the best locations on the surface to place the heat probe and seismometer. Over the next few weeks, InSight checked health indicators and monitor both weather and temperature conditions at the landing site.

= Landing site =

{{cleanup gallery|date=August 2024}}

File:PIA23376-Mars-InSightLander-MRO-View-20190923.jpg (23 September 2019)}}]]

File:PIA23140-Mars-InsightLander-Panorama-12092018.jpg

{{multiple image| caption_align=center|direction=horizontal|align=center|header=Views from the Mars InSight lander (animated) |width=

|image1=PIA25178-Mars-InSightLander-Sunrise-20220410.gif|caption1=Sunrise (April 2022)|width1=259|image2=PIA23180 cc-Mars-InSightLander-Clouds-Animated-20190425.gif|caption2=Clouds (April 2019)|width2=239|image3=PIA25178-Mars-InSightLander-Sunset-20220410.gif|caption3=Sunset (April 2022)|width3=239|footer=}}

{{multiple image

| align = center

| total_width = 800

| image1 = USGS-Mars-MC-15-ElysiumRegion-mola.png

| caption1 = InSight landing zone is in the south and west of this grid, near 4.5° North and 136° East, this is south and to the west of Elysium Mons and Eddie crater.

| image3 = PIA21489 - Advance Inspection of NASA's Next Mars Landing Site.jpg

| caption3 = The image footprints by HiRise on Mars Reconnaissance Orbiter for studying the planned Insight landing ellipse. From east to west the scale is about {{convert|100|mi|km|order=flip|abbr=on}}.

| image4 = PIA22878-Mars-InSightLander-FinalLocation-20181213.jpg

| caption4 =

InSight final landing location (red dot)
(13 December 2018)

}}

{{multiple image

| align = center

| total_width = 1000

| image1 = PIA22743-Mars-InSightLander-ArtistConcept-20181024.jpg

| caption1 = An artist's concept depicts NASA's InSight lander after it has deployed its instruments on the Martian surface

| image2 = PIA22892 Unlatching InSight's Arm.gif

| caption2 = The NASA's InSight spacecraft unlatched its robotic arm on 27 November 2018, the day after it landed on Mars.

| image3 = PIA22893 InSight's First View of Mars with the Cover Off.jpg

| caption3 = InSight on Mars − clear view (open lens cover) of landing area (ICC; 30 November 2018)

| image4 = PIA22875-InSightOnMarsSurface-ParachuteLanderHeatshield-20181211.jpg

| caption4 = InSight parachute, lander, shield (11 December 2018)

| image5 = PIA22875-InSightOnMarsSurface-ParachuteLanderHeatshield-20181126.jpg

| caption5 = InSight parachute, lander, shield (26 November 2018)

}}

As InSight{{'s}} science goals are not related to any particular surface feature of Mars, potential landing sites were chosen on the basis of practicality. Candidate sites needed to be near the equator of Mars to provide sufficient sunlight for the solar panels year round, have a low elevation to allow for sufficient atmospheric braking during EDL, be flat and relatively rock-free to reduce the probability of complications during landing, and have soft enough terrain to allow the heat flow probe to penetrate well into the ground.{{citation needed|date=May 2021}}

An optimal area that meets all these requirements is Elysium Planitia, so all 22 initial potential landing sites were located in this area. The only two other areas on the equator and at low elevation, Isidis Planitia and Valles Marineris, are too rocky. In addition, Valles Marineris has too steep a gradient to allow safe landing.

In September 2013, the initial 22 potential landing sites were narrowed down to four, and the Mars Reconnaissance Orbiter was then used to gain more information on each of the four potential sites before a final decision was made.{{r|landing|NBC2}} Each site consists of a landing ellipse that measures about {{convert|130|by|27|km|mi|abbr=on}}.

In March 2017, scientists from the Jet Propulsion Laboratory announced that the landing site had been selected. It is located in western Elysium Planitia at {{Coord|4.5|N|135.9|E|globe:mars_type:landmark|name=InSight landing site}}. The landing site is about {{convert|600|km|mi|abbr=on}} north from where the Curiosity rover is operating in Gale Crater.

On 26 November 2018, the spacecraft successfully touched down at its landing site, and in early December 2018 InSight lander and EDL components were imaged from space on the surface of Mars. The images provided precise position of the lander: {{Coord|4.5024|N|135.6234|E|globe:mars|format=dec}}.

{{multiple image |header=Mars InSight Lander – Self-portraits|align=center|caption_align=center|direction=horizontal|width= |image1=PIA22876-InSight-FirstSelfie-20181211.jpg|caption1=First (11 December 2018)|width1=200|image2=PIA23203-Mars-InSightLander-2ndSelfie-20190411.jpg|caption2=Second (11 April 2019)|width2=200 |image3=PIA25287-MarsInSightLander-DustySelfie-20220424.jpg |caption3=Third (24 April 2022) |width3=190 |image4=PIA25287-MarsInSightLander-BeforeAfterDustySelfies-20220523.gif |caption4=Before/After 1223 days of dust |width4=190 |footer=}}

Surface operations

On 26 November 2018, NASA reported that the InSight lander had landed successfully on Mars. The meteorological suite (TWINS) and magnetometer were operational, and the mission took approximately three months to deploy and commission the geophysical science instruments.{{r|insight-surface|nasa20181121}} After landing, the dust was allowed to settle for a few hours, during which time the solar array motors were warmed up and then the solar panels were unfurled.{{r|insight-solar|space.com3|insight-surface}} The lander then reported its systems' status, acquired some images, and it powered down to sleep mode for its first night on Mars. On its first sol on Mars it set a new solar power record of 4.6 kilowatt-hours generated for a single Martian day (known as a "sol"). This amount is enough to support operations and deploy the sensors.

{{multiple image

| align = center

| total_width = 800

| header = InSight on the surface of Mars (6 December 2018)

| image1 = PIA22871 Full View of InSight's Deck and Two Science Instruments.jpg

| caption1 =

Deck and science instruments

| image2 = PIA22872-Mars-InSight-20121206b.jpg

| caption2 =

Robotic arm over Martian soil

| image3 = PIA22873 Partial View of Insight's Robotic Arm and Deck.jpg

| caption3 =

Robotic arm and deck

| image4 = PIA22736 InSight Images a Solar Panel.jpg

| caption4 =

One of its two solar panels

| image5 = PIA22959-Mars-InSightLander-DeploysWind&ThermalShield-20190202.jpg

| caption5 =

Deployment of wind and thermal shield

| image6 = PIA23046-Mars-InSightLander-HeatProbeDeployment-20190212.jpg

| caption6 =

Deployment of heat probe (HP³)

| direction =

| alt1 =

}}

{{multiple image

| align = center

| direction = horizontal

| header = InSightseismometer deployed, first time onto the surface of another planet (19 December 2018)

| total_width = 800

| image1 = PIA22978-Mars-InSight-Lander-DeployingSeismometer-20181219.gif

| caption1 = The seismometer deployment animation from Instrument Context Camera

| image2 = PIA22977-Mars-InSight-Lander-DeployingSeismometer-IDC-20181219.gif

| caption2 = The seismometer deployment animation from Instrument Deployment Camera

| image3 = PIA22956-Mars-InSight-SeismometerDeployed-20181219.png

| caption3 = The seismometer deployed.

| image4 = PIA23177-Mars-InSightLander-Seismometer-20190423.jpg

| caption4 = The wind and thermal shield deployed over seismometer (Sol 110)

| image5 = PIA23043-Mars-InSightLander-Shield-FromSpace-20190204.jpg

| caption5 = The lander (green) and shield (white dot) – viewed from space (4 February 2019)

| alt1 =

}}

On 7 December 2018, InSight recorded the sounds of Martian winds with SEIS, which is able to record vibrations within human hearing range, although rather low (aka subwoofer-type sounds), and these were sent back to Earth. This was the first time the sound of Mars wind was heard after two previous attempts.

On 19 December 2018, the SEIS instrument was deployed onto the surface of Mars next to the lander by its robotic arm, and it was commissioned on 4 February 2019. After the seismometer became fully operational, the heat probe instrument was deployed on 12 February 2019.{{r|nasa20190213|eetasia1}}

In April 2019, NASA reported that the Mars InSight lander detected its first marsquake.{{r|nasa20190423|space.com4}}

File:NASA-Mars-InSightLander-MarsQuake-Seismometer-AV-20190406.webm; Sol 128; 6 April 2019)}}]]

In September 2019, researchers reported that InSight uncovered unexplained magnetic pulses, and magnetic oscillations.

On 24 February 2020, a summary of studies over the past year from InSight was presented which indicated that the planet Mars has active quakes, dust devils and magnetic pulses.{{r|nasa20200224|EA-20200224}}

File:PIA24664-MarsInSightLander-CleaningSolarPanel-20210522.webm

In February 2020, according to new data gathered from NASA's InSight lander, it was found that the Martian magnetic field at the landing site is about 10 times stronger than previously thought, and fluctuates rapidly.{{r|space.com5|teslarati1}}

In early 2021, the InSight team announced they would attempt to detect the arrival of the Mars 2020 mission using InSight's seismometers. Pre-landing modeling of the signals from Mars 2020's entry, descent and landing sequence suggested that the most probable source of any potential signal would be the impact of the spacecraft's cruise mass balance devices with the Martian surface, at speeds of around 4000 m/s.{{r|Fernando_2021|newsci1}} Shortly after successfully landing the Perseverance Rover, NASA announced that its landing went undetected by InSight. This helped demonstrate that Mars has a seismic efficiency of less than 3%.

On 12 April 2021, it was reported that Insight went into emergency hibernation because its solar panels were filled with Martian dust.

On 14 April, the lander began to transmit images after waking from hibernation.

On 3 May 2021, InSight used its robotic arm to trickle sand beside a solar panel. The InSight team wanted to let the sand blow away and touch the solar panels, sticking some dust particles to it, before leaving the solar panel. The sand trickle resulted in a boost in power of 30 watt-hours per sol.

In July 2021 three papers studying Mars's interior structure were published. Seismometer data confirms that the center of Mars is molten. The crust of Mars is thinner than expected and may have two or three sub-layers.

In January 2022, InSight went into safe mode due to a regional dust storm in the area, which caused a reduction in sunlight. During its time in safe mode, all but essential functions were suspended. It left safe mode on 19 January 2022 and resumed normal operations, however all science instruments were left off in the mean time.

As of May 2022, Insight has recorded 1,313 marsquakes.

The seismometer (SEIS), radio experiment (RISE) and the weather instruments (TWINS) continue to operate as the lander's Mars surface mission was extended by two years, until end of December 2022. The reason the mission was retired was due to insufficient power generation on the solar panels, due to dust accumulation.

In August 2024, a reservoir of liquid water was discovered on Mars – deep in the rocky outer crust of the planet. The findings came from a new analysis of seismometer data, which recorded four years' of vibrations – Mars quakes – from deep inside the Red Planet.{{Cite web |title=Mars water: Liquid water reservoirs found under Martian crust |url=https://www.bbc.com/news/articles/czxl849j77ko |access-date=2024-08-16 |website=www.bbc.com |language=en-GB}}{{Cite web |last=Strickland |first=Ashley |date=2024-08-12 |title=Oceans of water may be trapped deep beneath the Martian surface |url=https://edition.cnn.com/2024/08/12/science/mars-crust-water-reservoir-insight/index.html |access-date=2024-08-16 |website=CNN |language=en}}

=Heat Flow and Physical Properties Package=

On 28 February 2019, the Heat Flow and Physical Properties Package probe (mole) started digging into the surface of Mars. The probe and its digging mole were intended to reach a maximum depth of {{convert|5|m|ft|abbr=unit}} but it only went about {{convert|0.35|m|ft|abbr=unit}}, or three-quarters of the way out of its housing structure. After many attempts, the effort was given up as a failure in January 2021.

{{multiple image|align=center|direction=horizontal|header=InSight – Heat probe problem (June 2019)|total width=|image1=PIA23249-MarsInSightLander-DeployedHP3-20190212.jpg|caption1=Deploying probe |width1=112|image2=PIA23271-Mars-InSightLander-SignsOfHeatProbeShifting-20190304.jpg|caption2=Problem – signs of shifting|width2=199|image3=Insight's HP3 mole current position 5 June 2019.png |caption3=Current position|width3=116|image4=PIA23272-Mars-InSightLander-TestingSolutionsOnEarth-20190605.jpg|caption4=Testing solutions|width4=170|image5=PIA23276-Mars-InSightLander-TestingSolutionsToMoleProblemOnEarth-20190605.jpg|caption5=Possible solution|width5=200|image6=PIA23277-Mars-InSightLander-PreparingForHeatProbeSolution-20190601.gif|caption6=Prep for solution|width6=114 |image7=PIA23308-Mars-InSightLander-SavingTheMole-20190628.gif|caption7="Mole" uncovered|width7=114|footer=}}

{{multiple images

| align = center

| direction = horizontal

| total width =

| header = Mars InSight Lander - Attempts to solve mole problem

| image1 = PIA23379-MarsLander-InSight-HeatProbe-20191017.gif

| caption1 = "Pinning" helps to bury the mole. (17 October 2019)

| width1 = 210

| image2 = PIA23213-Mars-InSightLander-MoleBacksOutOfHole-20191026.gif

| caption2 = Mole partially backs out of the hole it made. (26 October 2019)

| width2 = 200

| image3 = PIA23512-Mars-InSightLander-MoleProbeTests-20191103.gif

| caption3 = Mole tests (3 November 2019)

| width3 = 200

| image4 = D000M0449 Mars InSight Mole push.png

| caption4 = Insight lander using its scoop to push on the back cap of the HP3 mole

| width4 = 200

| footer =

}}

In October 2019, the researchers at JPL concluded that the soil on Mars does not provide necessary friction for drilling, causing the mole to bounce around and form a wide pit around itself rather than dig deeper. They attempted a maneuver called {{Em|pinning}} in which they pressed the side of the scoop against the mole location to pin the side of the wall of the hole and increase friction. Pinning was initially successful, but then the mole backed out of its hole after a few weeks, suggesting the soil is accumulating below the mole.{{r|nasa20191027|CNET-20191027}}

In February 2020, the team reevaluated the risks of pushing the scoop directly against the back cap of the mole, and determined the procedure to be acceptable.

In June 2020, the team reported that the mole was finally underground, and was being evaluated to determine if the mole was able to dig as designed. On 9 July 2020, it was revealed that images taken on 20 June 2020 showed the mole bouncing again, indicating that it did not have sufficient friction to dig deeper. One suggested solution was to partially fill the hole with soil to increase friction.

File:PIA24263-MarsInsightLander-Mole-FinalEfforts-20210109.gif

By August 2020, the operations team had made some progress using the scoop to assist the mole in digging deeper into its hole, by pressing against the back. The scoop was used to fill the hole of the partially submerged mole, burying it fully for the first time. The team hoped the mole can now dig further into the surface on its own, possibly with the additional assistance of the scoop.

On 14 January 2021, the heat probe part of the mission was declared to be over, after the science team had determined that the soil properties at the landing location were incompatible with what the instrument had been designed for. The team attempted many different remedies over nearly two years to get the mole to burrow into the soil, but in the end, the attempts did not succeed. The friction between the soil and the probe was not enough for the mole to hammer itself down through the soil. Another set of attempts to get the probe deeper took place on 9 January 2021. After they proved unsuccessful, the decision was made to leave the probe as is and end attempts to dig deeper.

The mole did, with all the assisting measures, burrow itself completely underground. The top of the mole is 2 to 3 centimetres below the Martian surface. To be able to produce the intended scientific measurements, the mole needed to have dug itself at least 3 metres deep. Thus the mole was unsuccessful at producing its intended scientific results.

However the mole's operations did produce useful and interesting results about the soil at the InSight site; about conducting excavation, or drilling, on Mars; and about operating the lander's robotic arm through the mole-rescue efforts that used the arm in ways that were unplanned before the mission.

MarCO spacecraft

{{multiple image |align=right |direction=vertical|total_width=175

|image1=PIA20346marsco.jpg |caption1=Flight hardware of Mars Cube One (MarCO) (folded up)

|image2=PIA19388-Mars-InSight-MarCO-CubeSats-20150612.jpg |caption2=MarCO CubeSats relaying data during InSight{{'s}} landing (artist concept)

}}

{{Main|Mars Cube One}}

The Mars Cube One (MarCO) spacecraft are a pair of 6U CubeSats that piggybacked with the InSight mission to test CubeSat navigation and endurance in deep space, and to help relay real-time communications (with an eight-minute lightspeed delay) during the probe's entry, descent and landing (EDL) phase.{{r|space.com1|Dean2015}} The two 6U CubeSats, named MarCO A and B, are identical. They were launched along with InSight, but separated soon after reaching space, and they flew as a pair for redundancy while flanking the lander. They did not enter orbit, but flew past Mars during the EDL phase of the mission and relayed InSight{{'s}} telemetry in real time.{{r|space.com2|MarCO_JPL}} The success of the MarCO spacecraft proved the viability of the cubesat platform for deep space missions and helped serve as a technical demonstration for potential future missions of a similar nature. On 5 February 2019, NASA reported that the CubeSats went silent, and are unlikely to be heard from again.

  • Mass: {{convert|13.5|kg|lb|0|abbr=on}} each.
  • Dimensions: {{convert|30|x|20|x|10|cm|abbr=on}} each
  • Each has a reflectarray high gain antenna
  • Miniaturized radio operating in UHF (receive only) and X-band (receive and transmit).
  • They carry a miniature wide-angle camera.
  • Cold gas thrusters for attitude adjustments.
  • Star tracker for navigation.

Team and participation

File:NASA-TeamCheers-InSight-LandsOnThePlanetMars-20181126.jpg

The InSight science and engineering team includes scientists and engineers from many disciplines, countries and organizations. The science team assigned to InSight includes scientists from institutions in the U.S., France, Germany, Austria, Belgium, Canada, Japan, Switzerland, Spain, Poland and the United Kingdom.

Mars Exploration Rover project scientist W. Bruce Banerdt is the principal investigator for the InSight mission and the lead scientist for the SEIS instrument. Suzanne Smrekar, whose research focuses on the thermal evolution of planets and who has done extensive testing and development on instruments designed to measure the thermal properties and heat flow on other planets, is the lead for InSight{{'s}} HP3 instrument. The Principal Investigator for RISE is William Folkner at JPL. The SEIS Instrument

PI is Philippe Lognonné of IPGP, and the HP3 Instrument PI is Tilman Spohn of the DLR Institute of Planetary Research. The InSight mission team also includes project manager Tom Hoffman and deputy project manager Henry Stone.

Major contributing agencies and institutions are:

{{div col}}

{{div col end}}

File:Insight team at jpl-br2 (1).jpg

Name chips

As part of its public outreach, NASA organized a program where members of the public were able to have their names sent to Mars aboard InSight. Due to its launch delay, two rounds of sign-ups were conducted totaling 2.4 million names: 826,923 names were registered in 2015 and a further 1.6 million names were added in 2017. An electron beam was used to etch letters only {{frac|1|1000}} the width of a human hair (1 μm) onto {{convert|8|mm|in|1|abbr=on}} silicon wafers. The first chip was installed on the lander in November 2015 and the second on 23 January 2018.{{r|nasa20151217a|nasa20180124}}

{{multiple image |header=Name chips on InSight |align=center |width= |image1=PIA22540 InSight Camera Calibration Target, Laser Retroreflector, and Microchip.jpg|caption1=One name chip installed |width1=215|image2=PIA20164insightnamechip.jpg|width2=240|caption2=The first name chip for InSight |image3=PIA22236insightsecondchip.jpg|width3=200|caption3=The second name chip, inscribed with 1.6 million names, is placed on InSight in January 2018.|image4=Marsinsightdec72018idc.png|caption4=Name chips on Mars|width4=160}}

Gallery

PIA20278insightcausa.jpg|InSight lander loaded on a Boeing C-17 Globemaster III (December 2015)

PIA22232insightlandingonmars.jpg|InSight landing zone target with other NASA landing zones

Elysium Planitia labelled view.jpg|Global view of Mars. InSight landed in Elysium Plantia. Curiosity rover is in Gale crater.

InSight Profile of InSight entry, descent and landing events.jpg|Entry, Descent, and Landing sequence for InSight

PIA23278-Mars-InSightLanderTestSandbox-ActorBradPitt-20190906.jpg|Actor Brad Pitt visits the InSight test "sandbox" (September 2019).

PIA23349-Mars-InSightLander-RollingStonesRock-20181126.jpg|"Rolling Stones Rock"
a result from the landing
(November 2018)

{{multiple image |align=center|total_width=500

|header = Instrument Context Camera (ICC), November 2018

|image1=PIA22829 InSight's First Image from Mars.png|caption1=

First image from Mars, clear lens cap on

|image2=PIA22829 InSight's First Image from Mars, Annotated version.jpg|caption2=

First image with annotations

|image3=PIA22893 InSight's First View of Mars with the Cover Off.jpg|caption3=

Without clear lens cover

}}

See also

  • {{annotated link|Exploration of Mars}}
  • {{annotated link|List of missions to Mars}}

References

{{Reflist|refs=

{{Cite journal

| url= https://authors.library.caltech.edu/54355/2/jgr82msapp.pdf

| title= Signatures of Internally Generated Lander Vibrations

| journal= Journal of Geophysical Research

| author1= D. L. Anderson

| author2= W. F. Miller

| author3= G. V. Latham

| author4= Y. Nakamura

| author5= M. N. Toksöz

| author6= A. M. Dainty

| author7= F. K. Duennebier

| author8= A. R. Lazarewicz

| author9= R. L. Kovach

| author10= T. C. D. Knight

| display-authors= 5

| volume= 82

| issue= 28

| pages= 4524–4546; A–2

| date= 30 September 1977

| doi= 10.1029/JS082i028p04524

| bibcode= 1977JGR....82.4524A

| access-date= 31 January 2018

| archive-date= 1 February 2018

| archive-url= https://web.archive.org/web/20180201080008/https://authors.library.caltech.edu/54355/2/jgr82msapp.pdf

| url-status= live }}

{{cite news

| url= http://apnews.excite.com/article/20151222/us-sci--mars_lander-de6da5a926.html

| title= NASA calls off next Mars mission because of instrument leak

| work= Excite News

| agency= Associated Press

| date= 22 December 2015

| access-date= 22 December 2015

| archive-date= 23 December 2015

| archive-url= https://web.archive.org/web/20151223065409/http://apnews.excite.com/article/20151222/us-sci--mars_lander-de6da5a926.html

| url-status= dead }}

{{Cite news

| url= https://arstechnica.com/science/2012/08/new-probe-to-provide-insight-into-mars-interior/

| title= New probe to provide InSight into Mars' interior

| work= Ars Technica

| author1= Matthew Francis

| date= 21 August 2012

| access-date= 21 August 2012

| archive-date= 15 June 2018

| archive-url= https://web.archive.org/web/20180615190831/https://arstechnica.com/science/2012/08/new-probe-to-provide-insight-into-mars-interior/

| url-status= live }}

{{cite news

| url= https://www.smithsonianmag.com/air-space-magazine/cubesats-rescue-180955544/

| title= CubeSats to the Rescue?

| work= Smithsonian Air & Space Museum

| author1= Dirk Schulze-Makuch

| date= 9 June 2015

| access-date= 9 June 2015 }}

{{cite web

| url= http://www.orbitalatk.com/space-systems/space-components/solar-arrays/docs/FS007_15_OA_3862%20UltraFlex.pdf

| title= UltraFlex Solar Array Systems

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| access-date= 13 June 2015

| archive-date= 13 April 2016

| archive-url= https://web.archive.org/web/20160413045302/https://www.orbitalatk.com/space-systems/space-components/solar-arrays/docs/FS007_15_OA_3862%20UltraFlex.pdf

| url-status= live }}

{{cite news

| url= https://newatlas.com/nasa-insight-mars-names/52054/

| title= NASA probe to carry over 2.4 million names to Mars

| work= New Atlas

| author1= David Szondy

| date= 7 November 2017

| access-date= 8 January 2018

| archive-date= 27 November 2018

| archive-url= https://web.archive.org/web/20181127231510/https://newatlas.com/nasa-insight-mars-names/52054/

| url-status= live }}

{{cite web

| url= http://science.jpl.nasa.gov/people/Banerdt/

| title= JPL Science Division: People – Bruce Banerdt

| website= science.jpl.nasa.gov

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| website= nasa.gov

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| website= jpl.nasa.gov

| publisher= NASA / JPL

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{{cite news

| author1= Jia-Rui Cook

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| title= NASA's InSight Prepares to Take Mars' Temperature

| website= jpl.nasa.gov

| publisher= NASA / JPL

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| author1= Dwayne C. Brown

| author2= Alana Johnson

| author3= Andrew Good

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| date= 23 April 2019

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| publisher= NASA / JPL

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| website= jpl.nasa.gov

| publisher= NASA / JPL

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| title= Mars InSight's Mole Has Partially Backed Out of Its Hole

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| publisher= NASA

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{{cite news

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| title= NASA's InSight Reveals the Deep Interior of Mars

| date= 22 July 2021

| website= nasa.gov

| publisher= NASA

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| author1= Andrew Good

| author2= Karen Fox

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| title= NASA’s InSight Sees Power Levels Stabilize After Dust Storm

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| author2= Karen Fox

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| title= NASA's InSight Records Monster Quake on Mars

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| publisher= NASA

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| date= 20 September 2019

| work= National Geographic Society

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| title= Leaks in Instrument Force NASA to Delay Mars Mission Until 2018

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| newspaper= The New York Times

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| author1= Kenneth Chang

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| author1= Kenneth Chang

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{{cite news

| title= Opinion: Mars Beckons

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| date= 27 November 2018

| newspaper= The New York Times

| access-date= 28 November 2018

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{{cite news

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| title= NASA's InSight Mission Dies After 4 Years of Listening for Marsquakes

| url= https://www.nytimes.com/2022/12/21/science/nasa-mars-insight-mission.html

| date= 22 December 2022

| work= The New York Times

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{{cite news

| author1= Robin George Andrews

| title= A Radioactive Sea of Magma Hides Under the Surface of Mars

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| date= 25 October 2023

| work= The New York Times

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{{cite conference

| url= http://mepag.jpl.nasa.gov/meeting/2012-10/10_2012-1004_MEPAG.pdf

| title= InSight – Geophysical Mission to Mars

| conference= 26th Mars Exploration Program Analysis Group Meeting. 4 October 2012. Monrovia, California

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| access-date= 23 December 2022

| work= University of Oxford

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{{cite journal

| author1= M. Panning

| author2= P. Lognonne

| author3= B. Banerdt

| title= Planned Products of the Mars Structure Service for the InSight Mission to Mars

| journal= Space Science Reviews

| date= October 2017

| volume= 211

| issue= 1–4

| pages= 611–650

| doi= 10.1007/s11214-016-0317-5

| hdl= 10044/1/48928

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| bibcode= 2017SSRv..211..611P

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{{cite journal

| title= Localization of the InSight Lander

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| author2= M. P. Golombek

| author3= F. J. Calef

| author4= N. R. Williams

| author5= S. LeMaistre

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| author7= I. J. Daubar

| author8= D. Kipp

| author9= E. Sklyanskiy

| author10= H. Lethcoe-Wilson

| author11= R. Hausmann

| display-authors= 5

| date= March 2019

| journal= 50th Lunar and Planetary Science Conference, Held 18–22 March 2019 at the Woodlands, Texas. LPI Contribution No. 2132, Id.1948

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| page= 1948

| bibcode= 2019LPI....50.1948P

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{{cite web

| url= http://insight.jpl.nasa.gov/people/

| archive-url= https://web.archive.org/web/20120303133758/http://insight.jpl.nasa.gov/people/

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| title= InSight: People

| website= insight.jpl.nasa.gov

| publisher= NASA / JPL

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{{cite news

| author1= Bob Yirka

| title= Data from Insight reveals size of Mars's core

| url= https://phys.org/news/2021-03-insight-reveals-size-mars-core.html

| date= 19 March 2021

| website= Phys.org

| access-date= 19 March 2021

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| url= http://scienceinpoland.pap.pl/en/news/news,414002,polish-kret-will-fly-to-mars.html

| title= Polish Kret will fly to Mars

| work= Science in Poland

| date= 5 January 2017

| access-date= 1 May 2023 }}

{{cite web

| url= https://www.jpl.nasa.gov/news/press_kits/insight/launch/download/mars_insight_launch_presskit.pdf

| title= Mars InSight Launch Press Kit

| publisher= NASA / JPL

| date= May 2018

| access-date= 12 December 2018

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{{cite web

| url= http://www.cubesat-propulsion.com/cubesat-propulsion-delivery/

| title= VACCO delivers CubeSat propulsion system for JPL Mars Cube One (MarCO)

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| archive-date= 30 August 2018

| work= VACCO

| date= 2017 }}

{{cite web

| url= https://exploration.esa.int/web/mars/-/48898-edm-science-payload

| title= Schiaparelli Science Package and Science Investigations

| publisher= ESA

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{{cite news

| url= https://www.scientificamerican.com/article/nasa-rsquo-s-next-mars-lander-zooms-toward-launch/

| title= NASA's Next Mars Lander Zooms toward Launch

| work= Scientific American

| author1= Leonard David

| date= 14 November 2017

| archive-url= https://web.archive.org/web/20171114142155/https://www.scientificamerican.com/article/nasa-rsquo-s-next-mars-lander-zooms-toward-launch/

| archive-date= 14 November 2017

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{{cite web

| url= https://www.sciencedaily.com/releases/2018/10/181022171358.htm

| title= NASA's first image of Mars from a CubeSat

| archive-url= https://web.archive.org/web/20181128210723/https://www.sciencedaily.com/releases/2018/10/181022171358.htm

| archive-date= 28 November 2018

| work= Science Daily

| date= 18 October 2018

| access-date= 22 October 2018

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{{cite news

| url= https://www.spaceflightnow.com/news/n1312/19insight/

| title= Mars lander to launch from California on Atlas 5 in 2016

| work= Spaceflight Now

| author1= Stephen Clark

| date= 19 December 2013

| access-date= 20 December 2013

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{{cite news

| url= https://spaceflightnow.com/2016/03/05/fate-of-nasas-insight-mars-mission-to-be-decided-soon/

| title= Fate of NASA's InSight Mars mission to be decided soon

| work= Spaceflight Now

| author1= Stephen Clark

| date= 5 March 2016

| access-date= 9 March 2016

| archive-date= 16 November 2018

| archive-url= https://web.archive.org/web/20181116012749/https://spaceflightnow.com/2016/03/05/fate-of-nasas-insight-mars-mission-to-be-decided-soon/

| url-status= live }}

{{cite news

| url= https://spaceflightnow.com/2016/03/09/insight-mars-lander-escapes-cancellation-aims-for-2018-launch/

| title= InSight Mars lander escapes cancellation, aims for 2018 launch

| work= Spaceflight Now

| author1= Stephen Clark

| date= 9 March 2016

| access-date= 9 March 2016

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{{cite web

| author1= Stephen Clark

| url= https://spaceflightnow.com/2018/11/26/insight-tweaks-trajectory-to-home-in-on-mars-landing-site

| title= InSight tweaks trajectory to home in on Mars landing site

| work= Spaceflight Now

| access-date= 21 July 2019

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| url-status= live }}

{{cite web

| author1= Stephen Clark

| url= https://spaceflightnow.com/2019/02/04/insight-lander-seis-enclosure/

| title= InSight lander completes seismometer deployment on Mars

| archive-url= https://web.archive.org/web/20190214061702/https://spaceflightnow.com/2019/02/04/insight-lander-seis-enclosure/

| archive-date= 14 February 2019

| work= Spaceflight Now

| date= 4 February 2019

| access-date= 5 February 2019 }}

{{cite web

| url= https://science.jpl.nasa.gov/people/Smrekar/

| title= JPL Science Division: People – Sue Smrekar

| publisher= NASA / JPL

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| archive-url= https://web.archive.org/web/20180525024621/https://science.jpl.nasa.gov/people/Smrekar/

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{{cite press release

| url= http://solaerotech.com/emcore-awarded-solar-panel-manufacturing-contract-by-atk-for-nasas-insight-mars-lander-mission/

| title= SolAero Awarded Solar Panel Manufacturing Contract by ATK for NASA's InSight Mars Lander Mission

| work= SolAero

| date= 26 February 2014

| access-date= 13 June 2015

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{{cite news

| url= https://www.space.com/29374-nasa-cubesat-rocket-launch-system.html

| title= NASA Wants New Rocket Rides for Tiny CubeSats

| website= Space.com

| author1= Mike Wall

| date= 12 May 2015

| access-date= 13 May 2015

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{{cite news

| url= http://www.space.com/29489-marco-cubesats-mars-landing-2016.html

| title= Two Tiny 'CubeSats' Will Watch 2016 Mars Landing

| website= Space.com

| author1= Douglas Messier

| date= 27 May 2015

| access-date= 27 May 2015

| archive-date= 16 November 2018

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| url-status= live }}

{{cite web

| url= https://www.space.com/42607-insight-mars-lander-solar-power-record.html

| title= NASA's InSight Lander on Mars Just Set a Solar Power Record!

| author1= Sarah Lewin

| website= Space.com

| access-date= 9 December 2018

| date= 3 December 2018

| archive-date= 5 December 2018

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{{cite news

| author1= Meghan Bartels

| title= Marsquake! NASA's InSight Lander Feels Its 1st Red Planet Tremor

| url= https://www.space.com/insight-mars-lander-first-marsquake.html

| date= 23 April 2019

| website= Space.com

| access-date= 23 April 2019

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{{Cite web

| url= https://www.space.com/mars-weird-magnetic-field-insight-lander-discovery.html

| title= Mars lander reveals new details about the Red Planet's strange magnetic field

| author1= Elizabeth Howell

| website= Space.com

| date= 26 February 2020

| access-date= 28 February 2020

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{{cite news

| author1= Lee Cavendish

| url= https://www.space.com/42527-insight-mars-lander-journey-inside-red-planet.html

| title= Journey to the Center of the Red Planet: NASA's InSight Lander to Reveal the Secrets Inside Mars

| date= 25 November 2018

| website= Space.com

| access-date= 28 November 2018

| archive-date= 28 November 2018

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{{cite news

| url= https://www.space.com/18803-viking-2.html

| title= Viking 2: Second Landing on Mars

| website= Space.com

| author1= Elizabeth Howell

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{{cite web

| author1= Nora Taylor Tillman

| title= Details of the Moon's Core Revealed by 30-year-old Data

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{{cite news

| author1= Meghan Bartels

| title= The 'mole' on Mars is finally underground after a push from NASA's InSight lander

| url= https://www.space.com/insight-mars-lander-pushes-mole-into-red-planet.html

| date= 5 June 2020

| website= Space.com

| access-date= 6 June 2020

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{{cite news

| author1= Mike Wall

| title= The 'mole' on Mars from NASA's InSight lander may be stuck again

| url= https://www.space.com/nasa-insight-mars-lander-mole-stuck.html

| date= 9 July 2020

| website= Space.com

| access-date= 9 July 2020

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{{cite news

| url= https://www.space.com/28793-nasa-insight-mars-lander-landing-site.html

| title= NASA Eyeing Landing Site for 2016 Mars Mission

| website= Space.com

| author1= Mike Wall

| date= 11 March 2015

| access-date= 12 March 2015

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{{cite news

| url= https://www.space.com/26820-nasa-mars-insight-mission-planet-history.html

| title= NASA's Next Mars Lander Will Peer Deep Into Red Planet's History: Here's How

| website= Space.com

| author1= Leonard David

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{{cite web

| author1= Sarah Lewin

| url= https://www.space.com/42607-insight-mars-lander-solar-power-record.html

| title= NASA's InSight Lander on Mars Just Set a Solar Power Record!

| website= Space.com

| date= 30 November 2018

| access-date= 21 July 2019

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{{cite news

| author1= Tilman Spohn

| title= Mars InSight mission: The Mole is 'in' and the 'finishing touches' are 'in sight'

| url= https://www.dlr.de/blogs/en/desktopdefault.aspx/tabid-5893/9577_read-1144/

| date= 10 August 2020

| work= DLR Blog

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{{cite journal

| title= Bolide Airbursts as a Seismic Source for the 2018 Mars InSight Mission

| journal= Space Science Reviews

| author1= J. Stevanović

| author2= N. A. Teanby

| author3= J. Wookey

| author4= N. Selby

| author5= I. J. Daubar

| author6= J. Vaubaillon

| author7= R. Garcia

| display-authors=4

| volume= 211

| issue= 1–4

| pages= 525–545

| date= October 2017

| doi= 10.1007/s11214-016-0327-3

| bibcode= 2017SSRv..211..525S

| s2cid= 125102926

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| access-date= 30 September 2019

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{{cite thesis

| url= http://www3.imperial.ac.uk/pls/portallive/docs/1/30451696.PDF

| title= Design and Development of a Silicon Micro-Seismometer

| publisher= Imperial College London

| type= PhD

| author1= Sunil Kumar

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| access-date= 15 July 2015

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{{cite news

| url= http://www.tgdaily.com/space-features/55816-nasa-picks-project-shortlist-for-next-discovery-mission

| title= NASA picks project shortlist for next Discovery mission

| work= TG Daily

| author1= Kate Taylor

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| url= https://www.teslarati.com/nasa-insight-mars-magnetic-field-discovery/

| title= NASA's Mars Lander finds that the Red Planet's magnetic field is really weird

| author1= Amy Thompson

| date= 27 February 2020

| website= Teslarati.com

| access-date= 29 February 2020

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{{cite web

| title= Mars Microphones

| url= https://www.planetary.org/sci-tech/mars-microphones

| work= The Planetary Society

| access-date= 25 September 2020

| archive-date= 26 September 2020

| archive-url= https://web.archive.org/web/20200926080950/https://www.planetary.org/sci-tech/mars-microphones

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{{cite news

| url= http://www.thespacereview.com/article/2953/1

| title= InSight's Second Chance

| work= The Space Review

| author1= Jeff Foust

| date= 28 March 2016

| access-date= 5 April 2016

| archive-date= 15 June 2018

| archive-url= https://web.archive.org/web/20180615190736/http://www.thespacereview.com/article/2953/1

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{{cite tweet

| user= NASAInSight

| author= NASA InSight

| number= 1238497770228420608

| title= A bit of good news from #Mars: our new approach of using the robotic arm to push the mole appears to be working! The teams @NASAJPL/@DLR_en are excited to see the images and plan to continue this approach over the next few weeks. }}

{{cite news

| url= http://www.universetoday.com/93843/nasas-proposed-insight-lander-would-peer-to-the-center-of-mars-in-2016/

| title= NASA's Proposed 'InSight'Lander would Peer to the Center of Mars in 2016

| work= Universe Today

| author1= Ken Kremer

| date= 2 March 2012

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{{Cite web

| url= https://www.universetoday.com/14859/gravity-on-mars

| title= How Strong is the Gravity on Mars?

| work= Universe Today

| author1= Matt Williams

| date= 16 December 2016

| access-date= 9 December 2018

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{{cite news

| url= https://www.usatoday.com/story/tech/sciencefair/2013/09/04/mars-boring-landing/2764137/

| title= NASA searches for (literally) boring Mars landing site

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| author1= Dan Vergano

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{{cite web

| url= https://science.nasa.gov/science-news/science-at-nasa/2001/ast20jul_1/

| title= Happy (25th) Anniversary, Viking Lander

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{{cite news

| url= https://www.washingtonpost.com/national/health-science/nasa-will-send-robot-drill-to-mars-in-2016/2012/08/20/43bf1980-eaef-11e1-9ddc-340d5efb1e9c_story.html

| title= NASA will send robot drill to Mars in 2016

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| url-status= live }}

{{cite news

| author1= Robert Lee Hotz

| title= NASA's InSight Spacecraft Lands Safely on Mars

| newspaper= The Wall Street Journal

| date= 26 November 2018

| url= https://www.wsj.com/articles/nasas-insight-spacecraft-lands-safely-on-mars-1543263187

| access-date= 27 November 2018

| archive-date= 28 November 2018

| archive-url= https://web.archive.org/web/20181128134741/https://www.wsj.com/articles/nasas-insight-spacecraft-lands-safely-on-mars-1543263187

| url-status= live }}

{{YouTube

| id= o1ZlVGpyHXc

| title= Crazy Engineering: Space Claw on NASA's InSight Mars Lander }}

}}