What Is The Name Of Our Solar System?

Are you curious about the vast expanse beyond our world? The name of our solar system is the Solar System, aptly named after our star, the Sun. At WHAT.EDU.VN, we offer a wealth of information and resources to satisfy your curiosity. Dive in to explore planets, moons, asteroids, and other celestial objects within the Solar System.

1. What Defines Our Solar System?

Our solar system is a gravitationally bound system comprising the Sun and the objects that orbit it, either directly or indirectly. The objects that orbit the Sun directly, with the largest ones being the eight planets, are:

  • Mercury
  • Venus
  • Earth
  • Mars
  • Jupiter
  • Saturn
  • Uranus
  • Neptune

Numerous smaller objects, such as dwarf planets, asteroids, and comets, also populate our solar system. The Solar System extends far beyond the orbit of Neptune and includes the Kuiper Belt and the Oort Cloud.

2. What Is the Origin of the Name “Solar System?”

The name “Solar System” is derived from the Latin word “solaris,” meaning “of the Sun.” The Sun is the central star of our system, and it is the dominant gravitational force that governs the orbits of all the other celestial bodies within it. Therefore, it is natural to refer to our planetary system as the Solar System. According to NASA, the term “solar” is used to describe things related to our star, after the Latin word for Sun, “solis.”

3. Where Is Our Solar System Located in the Universe?

Our Solar System is located in the Milky Way Galaxy, a barred spiral galaxy that is estimated to contain hundreds of billions of stars. More specifically, we reside in one of the galaxy’s spiral arms, known as the Orion Arm or Orion Spur. The Solar System orbits the center of the Milky Way at a speed of approximately 515,000 mph (828,000 kph) and takes about 230 million years to complete one orbit around the galactic center.

4. What Are the Main Components of the Solar System?

The Solar System comprises several key components, each with unique characteristics:

  • The Sun: A yellow dwarf star, the Sun accounts for approximately 99.86% of the total mass of the Solar System. It provides the energy that sustains life on Earth.
  • Planets: The eight planets can be divided into two main categories: terrestrial planets (Mercury, Venus, Earth, and Mars) and gas giants (Jupiter and Saturn, ice giants Uranus and Neptune).
  • Dwarf Planets: These celestial bodies are smaller than the eight planets and include Pluto, Ceres, Eris, Makemake, and Haumea.
  • Moons: Many planets and dwarf planets have natural satellites, also known as moons, orbiting them.
  • Asteroids: These are rocky or metallic objects, mostly found in the asteroid belt between Mars and Jupiter.
  • Comets: Icy bodies that release gas and dust as they approach the Sun, creating a visible tail.
  • Kuiper Belt: A region beyond Neptune’s orbit containing numerous icy bodies, including Pluto.
  • Oort Cloud: A theoretical spherical cloud of icy objects located far beyond the Kuiper Belt, believed to be the source of long-period comets.

5. How Did the Solar System Form?

The Solar System formed approximately 4.6 billion years ago from a giant molecular cloud consisting of gas and dust. This cloud collapsed, possibly due to the shockwave of a nearby supernova. The collapse led to the formation of a solar nebula, a spinning, swirling disk of material. Most of the mass concentrated at the center, eventually forming the Sun. The remaining material in the disk coalesced to form the planets, moons, asteroids, and other objects in the Solar System.

6. What Are the Terrestrial Planets?

The terrestrial planets are the four innermost planets of the Solar System: Mercury, Venus, Earth, and Mars. They are characterized by their rocky surfaces, relatively high densities, and solid cores. These planets are closer to the Sun and have fewer or no moons compared to the gas giants.

7. What Are the Gas Giants?

The gas giants are the four outermost planets of the Solar System: Jupiter, Saturn, Uranus, and Neptune. They are significantly larger than the terrestrial planets and are primarily composed of hydrogen and helium. Jupiter and Saturn are known as gas giants, while Uranus and Neptune are classified as ice giants due to their higher concentrations of heavier elements like oxygen, carbon, nitrogen, and sulfur.

8. What Is the Asteroid Belt?

The asteroid belt is a region located between the orbits of Mars and Jupiter. It contains a vast number of irregularly shaped rocky and metallic objects called asteroids or minor planets. The asteroid belt is thought to be remnants from the early Solar System that never coalesced into a planet due to the gravitational influence of Jupiter.

9. What Is the Kuiper Belt?

The Kuiper Belt is a region beyond the orbit of Neptune, similar to the asteroid belt but much larger and more massive. It contains numerous icy bodies, including dwarf planet Pluto and other Kuiper Belt Objects (KBOs). The Kuiper Belt is thought to be the source of many short-period comets. NASA explains that the Kuiper Belt is a ring of icy bodies, almost all smaller than the most popular Kuiper Belt Object.

10. What Is the Oort Cloud?

The Oort Cloud is a theoretical spherical cloud of icy objects located far beyond the Kuiper Belt, at the outermost reaches of the Solar System. It is believed to be the source of long-period comets, which have highly elongated orbits and take thousands or even millions of years to orbit the Sun. The Oort Cloud is so distant that its existence is inferred from the orbits of comets rather than direct observation.

11. What Is the Heliosphere?

The heliosphere is a bubble-like region of space surrounding the Sun, created by the solar wind – a stream of charged particles emitted by the Sun. The heliosphere extends far beyond the orbits of the planets and protects the Solar System from interstellar radiation. The boundary where the solar wind is abruptly slowed by pressure from interstellar gases is called the termination shock.

12. Are There Other Solar Systems Besides Our Own?

Yes, there are many other solar systems beyond our own. These are called extrasolar systems or exoplanetary systems. Astronomers have discovered thousands of exoplanets orbiting other stars in our galaxy, the Milky Way. Some of these exoplanetary systems are very different from our Solar System, while others may have similarities.

13. How Do We Explore the Solar System?

We explore the Solar System using a variety of methods:

  • Telescopes: Ground-based and space-based telescopes allow us to observe celestial objects from a distance.
  • Spacecraft: Robotic spacecraft, such as orbiters, landers, and rovers, are sent to explore specific planets, moons, asteroids, and comets.
  • Space Probes: These are designed to travel long distances and study the outer regions of the Solar System, such as the Voyager probes, which have reached interstellar space.
  • Human Spaceflight: Although limited to the Moon so far, human spaceflight provides direct observation and exploration capabilities.

14. What Are Some Notable Space Missions to the Solar System?

Several notable space missions have significantly enhanced our understanding of the Solar System:

  • Voyager 1 and Voyager 2: These probes have explored the outer planets and are now in interstellar space.
  • Galileo: Studied Jupiter and its moons.
  • Cassini-Huygens: Explored Saturn and its moons, including the landing of the Huygens probe on Titan.
  • New Horizons: Visited Pluto and the Kuiper Belt.
  • Mars rovers (e.g., Curiosity, Perseverance): Exploring the surface of Mars and searching for signs of past or present life.

15. Is There Potential for Life on Other Worlds in Our Solar System?

The possibility of life on other worlds in our Solar System is a topic of ongoing scientific research. While no definitive evidence of life has been found, several locations are considered potentially habitable:

  • Mars: Evidence of past liquid water and the presence of organic molecules make Mars a prime target for life detection missions.
  • Europa (moon of Jupiter): A subsurface ocean of liquid water may harbor life.
  • Enceladus (moon of Saturn): Geysers erupting from Enceladus suggest a subsurface ocean with hydrothermal activity.
  • Titan (moon of Saturn): A unique environment with liquid methane seas and a thick atmosphere.

16. What Is the Significance of Studying the Solar System?

Studying the Solar System is essential for several reasons:

  • Understanding Our Origins: It helps us understand how our Solar System formed and how life originated on Earth.
  • Searching for Life Beyond Earth: It allows us to explore the possibility of life elsewhere in the Solar System.
  • Planetary Science: It provides insights into the geology, atmosphere, and climate of other planets and moons.
  • Resource Exploration: It may reveal potential resources that could be utilized for future space exploration.
  • Protecting Earth: Understanding asteroids and comets helps us assess and mitigate potential threats to our planet.

17. How Do We Name Celestial Objects in the Solar System?

The International Astronomical Union (IAU) is responsible for naming celestial objects in the Solar System. The IAU has established guidelines and procedures for naming planets, moons, asteroids, comets, and other features. The naming process often involves suggestions from discoverers, scientific teams, and the public, but the IAU has the final authority.

18. What Is the Future of Solar System Exploration?

The future of Solar System exploration is bright, with numerous missions planned or under development:

  • Europa Clipper: A NASA mission to study Europa and assess its habitability.
  • JUICE (Jupiter Icy Moons Explorer): An ESA mission to explore Jupiter and its icy moons Ganymede, Callisto, and Europa.
  • Artemis Program: NASA’s program to return humans to the Moon and establish a sustainable lunar presence.
  • Mars Sample Return: A joint NASA-ESA mission to collect samples from Mars and return them to Earth for analysis.
  • Venus Exploration: Missions to study Venus’s atmosphere and surface to understand its evolution and potential habitability.

19. How Does the Solar System Affect Earth?

The Solar System has a profound impact on Earth in many ways:

  • Sunlight: The Sun provides the energy that drives Earth’s climate, weather patterns, and photosynthesis in plants.
  • Gravity: The gravitational forces of the Sun and Moon influence Earth’s tides.
  • Asteroid and Comet Impacts: Impacts from asteroids and comets have shaped Earth’s geology and may have played a role in the evolution of life.
  • Space Weather: Solar flares and coronal mass ejections can disrupt Earth’s magnetic field and cause geomagnetic storms, affecting satellites and communication systems.
  • Orbital Variations: Changes in Earth’s orbit and axial tilt influence long-term climate patterns, such as ice ages.

20. What Are Some Unanswered Questions About the Solar System?

Despite the vast amount of knowledge we have gained about the Solar System, many questions remain unanswered:

  • How did life originate on Earth?
  • Is there life elsewhere in the Solar System?
  • What is the composition of the Oort Cloud?
  • How did the gas giants migrate to their current positions?
  • What is the nature of dark matter and dark energy in the Solar System?
  • How will the Sun evolve in the future, and how will it affect the Solar System?

21. What Is the Importance of Understanding Space Weather?

Understanding space weather is crucial because solar events can have significant impacts on Earth and our technological infrastructure:

  • Satellite Disruptions: Solar flares and coronal mass ejections can damage or disable satellites, affecting communication, navigation, and weather forecasting.
  • Power Grid Disruptions: Geomagnetic storms can induce currents in power grids, leading to blackouts and equipment damage.
  • Aviation Impacts: Radiation from solar events can pose a risk to airline passengers and crew, especially on polar routes.
  • Communication Interference: Solar activity can disrupt radio communication, affecting emergency services, aviation, and military operations.
  • GPS Errors: Geomagnetic disturbances can cause errors in GPS positioning, affecting navigation and surveying.

22. How Do Scientists Study the Composition of Planets and Moons?

Scientists use various methods to study the composition of planets and moons:

  • Spectroscopy: Analyzing the light reflected or emitted by a celestial object to determine its chemical composition.
  • Remote Sensing: Using instruments on spacecraft to measure the surface and atmospheric properties of planets and moons.
  • Sample Analysis: Analyzing samples collected from planets or moons, such as lunar rocks brought back by the Apollo missions or Martian soil analyzed by rovers.
  • Seismic Studies: Studying the interior structure of planets and moons by analyzing seismic waves generated by earthquakes or impacts.
  • Gravitational Measurements: Measuring the gravitational field of a planet or moon to determine its mass distribution and internal structure.

23. What Role Do Asteroids and Comets Play in the Solar System?

Asteroids and comets are remnants from the early Solar System and play several important roles:

  • Planetary Formation: They provide insights into the building blocks of planets and the processes that shaped the Solar System.
  • Delivery of Water and Organic Molecules: Comets may have delivered water and organic molecules to Earth, contributing to the origin of life.
  • Impact Events: Asteroid and comet impacts have shaped the geology and evolution of planets and moons.
  • Potential Resources: Asteroids may contain valuable resources, such as metals and water, that could be utilized for future space exploration.
  • Scientific Study: They provide opportunities to study the composition and history of the early Solar System.

24. How Does the Study of Exoplanets Enhance Our Understanding of the Solar System?

The study of exoplanets, planets orbiting other stars, has revolutionized our understanding of planetary systems:

  • Diversity of Planetary Systems: Exoplanet discoveries have revealed a wide diversity of planetary systems, challenging our assumptions about how planetary systems form and evolve.
  • Habitability: The search for habitable exoplanets has expanded our understanding of the conditions necessary for life to arise.
  • Planetary Migration: Exoplanet studies have provided evidence for planetary migration, where planets can move from their initial orbits to different locations in their systems.
  • Comparative Planetology: Comparing exoplanets with planets in our Solar System helps us understand the factors that determine a planet’s characteristics and habitability.
  • Technological Advancements: The search for exoplanets has driven the development of new technologies for detecting and characterizing planets orbiting other stars.

25. What Is the Connection Between the Solar System and the Search for Extraterrestrial Intelligence (SETI)?

The Solar System and the search for extraterrestrial intelligence (SETI) are connected in several ways:

  • Potential Habitable Environments: The Solar System provides potential environments where extraterrestrial life could exist, such as Mars, Europa, and Enceladus.
  • Probes for Detecting Life: Missions to these locations could search for signs of past or present life, providing valuable information for SETI efforts.
  • SETI Targets: Exoplanets discovered through exoplanet surveys are potential targets for SETI programs, which search for radio signals or other signs of intelligent life.
  • Understanding Habitability: Studying the Solar System helps us understand the conditions necessary for life to arise and evolve, informing the search for habitable exoplanets.
  • Technological Development: The technologies developed for exploring the Solar System and searching for exoplanets can also be used for SETI research.

26. How Do Tides Work Within Our Solar System?

Tides on Earth are primarily caused by the gravitational pull of the Moon and, to a lesser extent, the Sun. Here’s how it works:

  • Gravitational Attraction: The Moon’s gravity pulls on the Earth, causing the water on the side of Earth closest to the Moon to bulge out towards it. This bulge is a high tide.
  • Inertia: On the opposite side of the Earth, inertia causes another bulge as the Earth is also being pulled towards the Moon. This results in another high tide on the opposite side.
  • Earth’s Rotation: As the Earth rotates, different locations pass through these bulges, resulting in high and low tides.
  • Sun’s Influence: The Sun also exerts a gravitational force on Earth, but its effect is about half that of the Moon due to its greater distance. When the Sun, Earth, and Moon are aligned (during new and full moons), the combined gravitational forces result in higher tides, known as spring tides. When the Sun and Moon are at right angles to each other (during quarter moons), their gravitational forces partially cancel out, resulting in lower tides, known as neap tides.

While tides are most noticeable on Earth’s oceans, tidal forces also affect other celestial bodies in the Solar System, such as moons orbiting planets.

27. How Are Impact Craters Formed in Our Solar System?

Impact craters are formed when asteroids, comets, or meteoroids collide with the surface of a planet, moon, or other celestial body. Here’s the process:

  • Collision: A space rock traveling at high speed strikes the surface of a celestial body.
  • Compression: The impact creates intense pressure and heat, compressing the surface material.
  • Excavation: The force of the impact excavates a large volume of material, creating a bowl-shaped depression.
  • Ejection: Material is ejected from the crater in all directions, forming a blanket of debris around the impact site.
  • Modification: Over time, the crater may be modified by erosion, volcanism, or other geological processes.

The size and shape of an impact crater depend on the size and velocity of the impactor, as well as the composition and structure of the target surface. Impact craters are common features on many planets and moons in the Solar System, providing evidence of past collisions.

28. How Is the Magnetic Field Created in the Solar System?

Magnetic fields are generated by the movement of electrically conductive material within a celestial body. Here’s how it works for different objects in the Solar System:

  • Sun: The Sun’s magnetic field is generated by the movement of plasma in its interior, a process known as the solar dynamo. The Sun’s magnetic field is complex and dynamic, with magnetic field lines twisting and tangling, leading to solar flares and coronal mass ejections.
  • Earth: Earth’s magnetic field is generated by the movement of molten iron in its outer core, a process known as the geodynamo. The Earth’s magnetic field protects the planet from harmful solar wind and cosmic radiation.
  • Other Planets: Some other planets in the Solar System, such as Jupiter and Saturn, also have magnetic fields generated by internal dynamos.
  • Moons: Some moons, such as Ganymede, also have magnetic fields, possibly generated by similar dynamo processes.

The strength and orientation of a magnetic field depend on the size, composition, and rotation rate of the celestial body, as well as the properties of the conductive material within it.

29. How Are Auroras Formed in Our Solar System?

Auroras, also known as the Northern Lights (Aurora Borealis) and Southern Lights (Aurora Australis), are caused by the interaction of charged particles from the Sun with a planet’s magnetic field and atmosphere. Here’s the process:

  • Solar Wind: The Sun emits a stream of charged particles known as the solar wind.
  • Magnetic Field Interaction: When the solar wind reaches a planet with a magnetic field, such as Earth, the magnetic field deflects most of the particles. However, some particles are channeled along the magnetic field lines towards the poles.
  • Atmospheric Collision: The charged particles collide with atoms and molecules in the planet’s atmosphere, exciting them to higher energy levels.
  • Emission of Light: When the excited atoms and molecules return to their normal energy levels, they emit light in various colors, creating the auroral display.

Auroras are most commonly observed near the poles because the magnetic field lines converge there. The color of the aurora depends on the type of atom or molecule that is excited, with oxygen producing green and red light, and nitrogen producing blue and purple light.

30. How Are Rings Formed Around Planets in Our Solar System?

Planetary rings are formed by various processes, including:

  • Tidal Disruption: When a moon or other celestial body gets too close to a planet, the planet’s tidal forces can tear it apart, creating a ring of debris.
  • Impacts: Collisions between moons or other objects can create debris that forms a ring.
  • Volcanic Activity: Volcanic eruptions on moons can eject material into space, contributing to ring formation.
  • Capture: A planet can capture a passing asteroid or comet, which then becomes part of a ring system.

The composition of planetary rings can vary depending on the source of the material. For example, Saturn’s rings are primarily composed of ice particles, while Uranus’s rings are darker and contain more rock and dust.

31. How is the Age of the Solar System Determined?

The age of the Solar System is primarily determined through radiometric dating of meteorites. Meteorites are remnants of the early Solar System and provide valuable information about its formation. Here’s the process:

  • Radiometric Dating: This technique involves measuring the decay of long-lived radioactive isotopes in meteorites. Radioactive isotopes decay at a constant rate, and by measuring the ratio of the parent isotope to the daughter isotope, scientists can determine how long ago the meteorite formed.
  • Isotopes Used: Common isotopes used for dating include uranium-238, uranium-235, thorium-232, potassium-40, and rubidium-87.
  • Dating Meteorites: Scientists analyze various types of meteorites, including chondrites and achondrites, which have different compositions and formation histories. By dating multiple meteorites, they can obtain a consistent age for the Solar System.
  • Age of the Solar System: The age of the Solar System, as determined by radiometric dating of meteorites, is approximately 4.568 billion years. This age is consistent with other estimates based on the age of the Sun and the evolution of stars.

32. What Are the Lagrange Points in the Solar System?

Lagrange points are locations in space where the gravitational forces of two large bodies, such as the Sun and Earth, balance each other out. At these points, a smaller object can remain relatively stable with respect to the two larger bodies. There are five Lagrange points in any two-body system, labeled L1 through L5:

  • L1: Located between the two large bodies, along the line connecting them. Objects at L1 can remain in a stable orbit relative to the two bodies.
  • L2: Located beyond the smaller of the two large bodies, along the line connecting them. Objects at L2 can also remain in a stable orbit.
  • L3: Located beyond the larger of the two large bodies, along the line connecting them. L3 is less stable than L1 and L2.
  • L4 and L5: Located at the vertices of two equilateral triangles, with the two large bodies at the other vertices. L4 and L5 are stable points, and objects can remain there for long periods of time.

Lagrange points are useful locations for placing spacecraft and observatories because they require minimal energy to maintain their positions.

33. What Makes Earth Unique in the Solar System?

Earth is unique in the Solar System for several reasons:

  • Liquid Water: Earth is the only planet in the Solar System with stable bodies of liquid water on its surface. Water is essential for life as we know it.
  • Oxygen-Rich Atmosphere: Earth has an atmosphere rich in oxygen, which is produced by photosynthetic organisms. Oxygen is essential for the respiration of many organisms.
  • Plate Tectonics: Earth is the only planet in the Solar System with active plate tectonics. Plate tectonics play a crucial role in regulating Earth’s climate and maintaining its habitability.
  • Life: Earth is the only planet in the Solar System known to harbor life. Life has transformed Earth’s atmosphere, oceans, and land surface.
  • Habitable Zone: Earth is located in the habitable zone of the Solar System, where temperatures are suitable for liquid water to exist on its surface.

34. What are the Challenges of Interstellar Travel?

Interstellar travel, traveling between stars, faces immense challenges:

  • Distance: The vast distances between stars mean travel times would be extremely long, potentially thousands of years.
  • Speed: Reaching even a fraction of the speed of light, necessary to make interstellar travel feasible, requires enormous amounts of energy.
  • Energy: Current propulsion systems are not capable of generating the energy needed for interstellar travel. Fusion or antimatter propulsion are theoretical possibilities but pose significant technical challenges.
  • Radiation: Interstellar space is filled with high-energy radiation that can damage spacecraft and pose a risk to human health.
  • Navigation: Navigating across interstellar distances with sufficient accuracy is a major challenge.
  • Communication: Communicating with spacecraft over interstellar distances would be difficult due to signal delay and signal degradation.
  • Cost: The cost of interstellar travel would be astronomical, requiring a massive investment of resources.

Despite these challenges, scientists and engineers are exploring various technologies that could potentially enable interstellar travel in the future.

35. What Is the Drake Equation and Its Significance?

The Drake equation is a probabilistic argument used to estimate the number of active, communicative extraterrestrial civilizations in the Milky Way galaxy. It was formulated by Frank Drake in 1961 and is expressed as:

N = R* ⋅ fp ⋅ ne ⋅ fl ⋅ fi ⋅ fc ⋅ L

Where:

  • N = The number of civilizations in the Milky Way galaxy with which communication might be possible.
  • R* = The average rate of star formation in our galaxy.
  • fp = The fraction of those stars that have planets.
  • ne = The average number of planets that can potentially support life per star that has planets.
  • fl = The fraction of planets that actually develop life at some point.
  • fi = The fraction of planets with life that actually develop intelligent life.
  • fc = The fraction of civilizations that develop a technology that releases detectable signs into space.
  • L = The average length of time for which such civilizations release detectable signals into space.

The Drake equation is not meant to provide a definitive answer to the number of extraterrestrial civilizations, but rather to stimulate discussion and research on the factors that determine the likelihood of life beyond Earth.

36. How Do We Search for Exoplanets?

Scientists use several methods to search for exoplanets, planets orbiting other stars:

  • Transit Method: This method involves measuring the dimming of a star’s light as a planet passes in front of it. The transit method is used by missions such as Kepler and TESS.
  • Radial Velocity Method: This method involves measuring the wobble of a star as it is gravitationally tugged by an orbiting planet.
  • Direct Imaging: This method involves directly imaging exoplanets using powerful telescopes. Direct imaging is challenging because exoplanets are faint and close to their host stars.
  • Gravitational Microlensing: This method involves using the gravity of a star to magnify the light of a background star. If a planet is orbiting the foreground star, it can produce a characteristic brightening of the background star’s light.
  • Astrometry: This method involves measuring the precise position of a star over time. If a star has a planet orbiting it, the star will wobble slightly in its position.

Each of these methods has its own advantages and limitations, and astronomers often use multiple methods to confirm the existence of exoplanets.

37. What is the Habitable Zone?

The habitable zone, also known as the Goldilocks zone, is the region around a star where temperatures are suitable for liquid water to exist on the surface of a planet. Liquid water is considered essential for life as we know it, so planets in the habitable zone are considered the most likely candidates for harboring life. The location of the habitable zone depends on the size and temperature of the star. Smaller, cooler stars have habitable zones closer to them, while larger, hotter stars have habitable zones farther away.

38. What Are the Future Missions Planned for the Solar System?

Several exciting missions are planned for future exploration of the Solar System:

  • Europa Clipper: A NASA mission to study Europa, one of Jupiter’s moons, and assess its potential habitability.
  • JUICE (Jupiter Icy Moons Explorer): An ESA mission to explore Jupiter and its icy moons Ganymede, Callisto, and Europa.
  • Dragonfly: A NASA mission to explore Titan, Saturn’s largest moon, and search for prebiotic chemistry.
  • Artemis Program: NASA’s program to return humans to the Moon and establish a sustainable lunar presence.
  • Mars Sample Return: A joint NASA-ESA mission to collect samples from Mars and return them to Earth for analysis.
  • VERITAS (Venus Emissivity, Radio Science, InSAR, Topography, and Spectroscopy): A NASA mission to map the surface of Venus and study its geology.

These missions promise to provide new insights into the Solar System and our place in the universe.

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