Yes, both the earth and moon have rilles. A rille can be defined as a small brook (as on Earth) and as a long narrow straight valley on the moon's surface.
A maria , highlands, rilles, and ray craters
Yes, there are valleys on the moon called rilles or sinuous rilles. They are long, winding valleys that were likely formed by ancient lava flows or collapsed lava tubes. One of the most famous lunar valleys is Vallis Schröteri, located near the Aristarchus Plateau.
There are no active volcanoes on the moon, but there are volcanic features like lava tubes, domes, and rilles believed to have originated from past volcanic activity. Some of these features include Mons Huygens, Mons Bradley, and Mons Rümker.
A channel on the moon is called a rille, which is a long, narrow valley that can range from a few hundred meters to several kilometers in width and can extend for hundreds of kilometers in length. Rilles are believed to have formed from ancient lava flows or collapsed lava tubes.
Craters are one of the moon's landforms. Another lunar landform is a maria, which is what Galileo called the lowland areas of the moon because he thought that they were covered in water (maria is Latin for sea).
A maria , highlands, rilles, and ray craters
Cracks in the moon's bedrock are called "faults" or "fractures." These features are caused by stress and movement within the lunar surface, much like on Earth.
Some landforms found on the moon that Earth does not have include impact craters of various sizes, such as lunar mare basins and rays, formed by meteoroid impacts. Additionally, the moon features lava tubes and rilles, which are long, deep valleys formed by ancient volcanic activity.
Trenches on the moon are called rilles, and they are thought to be long, narrow depressions carved by lava flows or collapsed lava tubes. Rilles can stretch for hundreds of kilometers across the lunar surface, providing clues to the moon's volcanic past and geologic history. These features are a common and intriguing aspect of the moon's landscape.
Moon craters are mostly formed by impacts from meteoroids, asteroids, or comets striking the moon's surface. Rilles, on the other hand, are thought to be formed by lava tubes or collapsed lava channels from ancient volcanic activity. Both features give us information about the moon's geological history.
The long deep cracks in the Maria Bedrock on the Moon are called rilles. These are narrow, trench-like depressions that can be several kilometers wide and hundreds of kilometers long. Rilles are thought to have formed from a combination of volcanic and tectonic processes.
rilles
They are narrow trenches or small, narrow valleys.
Maria, terrae and sinuous rilles.
i love marshmello rilles
Ridges, rilles, craters and regoliths
They may be known as faults, joints or more generally as discontinuities. Please see the related links for more information.