The field of exoplanet study has come a long way in recent decades. To date, 5,063 exoplanets have been confirmed in 3,794 systems beyond our own, with another 8,819 candidates awaiting confirmation. In the coming years, tens of thousands of more planets are expected to be found, thanks to next-generation observatories. The ultimate goal in this search is to find planets that are "Earth-like," meaning they have a good chance of supporting life. This is no easy task, as rocky planets located within their parent star's habitable zones (HZs) tend to orbit closely, making them harder to see.

To make this process easier, NASA is designing a hybrid observatory consisting of a "Starshade" that will block out a star's light so that a ground-based telescope can directly image planets orbiting it.

Planetary scientists from Rice University, NASA's Johnson Space Center and the California Institute of Technology have an answer to a mystery that's puzzled the Mars research community since NASA's Curiosity rover discovered a mineral called tridymite in Gale Crater in 2016.

Tridymite is a high-temperature, low-pressure form of quartz that is extremely rare on Earth, and it wasn't immediately clear how a concentrated chunk of it ended up in the crater. Gale Crater was chosen as Curiosity's landing site due to the likelihood that it once held liquid water, and Curiosity found evidence that confirmed Gale Crater was a lake as recently as 1 billion years ago.