About Planetary Analogs
Similar environments on different worlds are called planetary analogs. Studying planetary analogs is a powerful way to make sense of our solar system.
Studying Earth to Understand Other Worlds
The quest to understand our solar system begins close to home. Earthquake science paves the way for the study of quakes on the Moon, Mars, and icy ocean worlds. Our planet's driest deserts serve as testing grounds in the search for life on Mars, and prepare us to think about life elsewhere in the universe. Field research on Earths' volcanoes helps us interpret evidence of volcanic activity on the Moon, Mars, Venus, and beyond.
Similar Landscapes, Different Worlds
Cooled Lava on Earth and the Moon
Geologic Analogs
Rocks record history. They tell the stories of past volcanic eruptions, giant earthquakes, erosion processes, and meteoric impacts – if we know how to look. To make sense of what we see, we study geology from many different perspectives.
Remote sensing shows us the big picture. Large features like canyons and continents are easy to see from far away. Spacecraft, aircraft, drones, and telescopes are all useful remote sensing tools.
Sometimes, it helps to take a closer look. Information collected on site, in the field, is called ground truth data. Apollo astronauts have collected ground truth data on the Moon. Robotic landers and rovers can make ground truth observations, too.
Ground truth science on Earth provides valuable information about our home planet. It also helps us to check our understanding of satellite imagery. When long-distance observations of Earth match with data gathered on the ground, we can be confident about using remote sensing on other worlds, too.
Into The Field With NASA: Valley Of Ten Thousand Smokes
To better understand Mars, NASA's Goddard Instrument Field Team headed deep into the backcountry of Katmai National Park.
Read the Story![Seven people, with large backpacks, hiking down a hill of lumpy snow dusted with beige volcanic ash. Behind them is a steep wall of dirt with streaks of fresh green shrubbery. The people appear tiny against the landscape and are all in the left half of the image. On the right are overlapping views of three distinct geological formations: a light-colored slope in the foreground, a tan and orange river gorge in the middle ground, and snow-capped mountains in the background, under a partly cloudy sky.](https://science.nasa.gov/wp-content/uploads/2024/07/vtts1-hikeoutlandscape.jpg?w=4096&format=jpeg)
Volcanism
Different kinds of eruptions create a variety of volcanoes. Explosive eruptions make ash. Gentler eruptions generate lava flows. Some lava flows also form caves, called lava tubes. Explorers are curious about lava tubes because they can harbor resources like water and sulfur. Future visitors to the Moon might use lava tubes for shelter from the hazards of outer space.
Researchers visit lava tubes on Earth to test new ways to identify them from the surface. They use special science instruments like Ground Penetrating Radar, magnetic field detectors, and seismometers to "see through" the rock and detect caves below. One day, astronauts could use tools like these to study lava flows on the Moon and Mars.
Erosion
The movement of materials like dust, sand, and rocks around the surface of a planet is called erosion. Wind, storms, landslides, glaciers, and flowing water all cause this kind of movement. To find out what kind of erosion has happened, scientists study the patterns left behind. On Mars, for example, ancient shorelines and dry riverbeds hint at a watery past.
Similar Landscapes, Different Worlds
Wind-blown dunes on Earth and Titan
Tectonism
Terrestrial planets begin as molten bodies and cool over time. As a planet loses heat, its surface changes shape. Hot material continues to move around in the planet’s interior, causing surface deformation. This is called tectonism.
Tectonic activity is all around us. Mountains, faults, folds, fractures, and earthquakes teach us about Earth's past and present. Lunar experiments set up by Apollo astronauts show that the Moon is not only quaking, but shrinking. Marsquakes reveal the Red Planet’s internal structure to NASA's InSight lander. Each world provides clues about how objects in our solar system formed, how they cooled, and what might be happening inside.
Ocean Worlds Analog
Science on Ice
Northwest Greenland
Researcher Angela Marusiak uses seismometers to record vibrations from a hammer strike by a colleague. The detectors are sensitive enough to measure earthquakes thousands of miles away. Tests like this one pave the way for future measurements of moonquakes on icy worlds like Jupiter’s moon Europa. Credit: NASA/Namrah Habib
Impact
Impacts batter planetary surfaces throughout our solar system. Often, when an object traveling through space crashes into a planet or moon, it forms a crater. In very large impacts, surface material can be excavated, or thrown from the impact site. This leaves a window for scientists to see what lies beneath.
Earth has relatively few impact craters. Many objects collide with the Moon or burn up in the atmosphere before hitting the ground. When impactors do reach Earth’s surface, our active planet slowly erases the evidence. Erosion, tectonic movement, and volcanic activity make ancient craters difficult to see.
Despite these factors, a few impact sites remain visible and accessible on Earth's surface. These examples help geologists interpret craters on the Moon, Mars, and beyond.
Similar landscapes, different worlds
Impact craters on Earth and the Moon
Impact sites on Earth can tell us about the history encoded in craters on other worlds.
Astrobiology Analogs
Astrobiologists explore the forms that biology might take on other worlds. Our planet’s most extreme habitats are full of surprising examples to study. Deep in Earth's oceans, for instance, microbes thrive in very salty, high-pressure environments. These tough and tiny creatures show us what life could be like in salt-watery alien terrain.
The search for extraterrestrial life requires both evidence and imagination. It’s difficult to predict what an encounter with life beyond Earth will be like. There is no guarantee that it will resemble anything humans have ever experienced. Will we know it when we see it? Will we find biosignatures in rocks, in an atmosphere if there is one, in liquid form? Could a close-up image provide proof? Will we need to examine the area in other ways? Is it possible to study alien biology while keeping it, and our own world, safe from harm?
Earth's strangest ecosystems prepare us to ask the right questions when searching for life in other places.
Mission Analogs
Before Apollo astronauts collected samples on the Moon, they practiced here on Earth. Today, teams test their plans and equipment in environments ranging from volcanic fields to the ocean floor. Future crews, too, will train on Earth for the challenges of space travel. This kind of preparation is called analog mission research.
Analog missions allow us to try out equipment and procedures in rough, remote places without ever leaving our planet. Some teams spend up to three weeks at a time living and working deep undersea. Others take to the desert to try out new rovers and geological tools. These trials reveal strengths and weaknesses so that we can improve our systems. They also teach us how to manage human challenges like prolonged isolation.
Putting the Pieces Together
In the field, everyone works together to achieve mission goals. Astronauts may try new exploration tools while geologists search for hints about our planet's past. Engineers can test their rovers against rough terrain and time delays. At the same time, astrobiologists might scour the rocks nearby for evidence of past and present life.
Analog studies have already changed the way we understand our place in space, and there are many discoveries left to make. Future scientists, engineers, and astronauts will have exciting questions to answer. To succeed, they'll need to learn all they can from each other and our home planet.