3001970

3001970 is a small asteroid located in the inner region of the asteroid belt, between the orbits of Mars and Jupiter. It was discovered on October 1, 1980, by American astronomer Edward Bowell at the Anderson Mesa Station of the Lowell Observatory in Arizona. The asteroid is classified as a main-belt asteroid, which means it orbits the Sun in the same region as most other asteroids.

3001970 has an estimated diameter of approximately 2 kilometers. Its orbit is relatively stable, with an orbital period of about 3.6 Earth years. The asteroid's semi-major axis is 2.37 astronomical units (AU), and its eccentricity is 0.13. The inclination of its orbit to the ecliptic plane is 11.3 degrees.

The spectral type of 3001970 is not well-determined, but it is likely to be a C-type asteroid, which are carbonaceous and typically found in the outer regions of the asteroid belt. The surface of 3001970 is likely covered in dark, carbon-rich material, giving it a low albedo.

As of now, there are no known moons or companions orbiting 3001970. The asteroid's rotation period is not well-known, but it is likely to be in the range of a few hours to a few days. The asteroid's absolute magnitude is 15.6, which is a measure of its brightness.

3001970 is not a near-Earth object, meaning it does not pose a threat to Earth. It is also not a target for any planned space missions. However, its study can provide valuable insights into the composition and evolution of the asteroid belt.