highlands
Lava flows.
The presence of maria on the Moon's surface indicates that those areas were formed by ancient volcanic activity. They are characterized by smoother, darker plains and are believed to have been created by lava flows millions of years ago.
Maria are large, dark, basaltic plains on the Moon's surface that were formed by ancient volcanic activity. They are made up of solidified lava flows and are relatively flat compared to the rugged highlands that make up the rest of the lunar surface.
The moon surface features that probably formed when lava flows filled large basins are called maria, which are large, dark plains visible from Earth. These maria were created by ancient volcanic activity that filled the low-lying basin areas with basaltic lava flows.
Those are likely basaltic lava fields called "lava fields" or "lava beds." These areas are created when lava flows and cools to form a hardened surface. They can resemble oceans because of their dark color and often expansive appearance.
Io, one of Jupiter's moons, does not have many impact craters on its surface because its surface is constantly being resurfaced by volcanic activity. The geologically active nature of Io means that the lava flows and volcanic eruptions continuously erase any impact craters that may form on its surface.
This type of water is called surface runoff. It occurs when rainwater or snowmelt flows over the ground surface, unable to penetrate into the soil or evaporate. Surface runoff can accumulate in rivers, lakes, and oceans or contribute to flooding in urban areas.
The South Pole
When lava flowed over the Moon's surface, it formed vast plains known as maria. These are flat, dark areas that were created by ancient volcanic activity on the Moon. The lava flows filled in large impact basins, creating the smooth, dark patches we see on the lunar surface.
Forever Flows was created in 2006.
As Blood Flows was created in 1993.
My River Flows was created in 2005.