They are narrow trenches or small, narrow valleys.
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.
Yes, Earth has rilles, which are long, narrow valleys or channels on the surface. Rilles are often created by flowing lava or water erosion. An example of rilles on Earth can be seen in the Moon-like landscape of the volcanic island of Lanzarote in the Canary Islands.
Maria, terrae and sinuous rilles.
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.
A maria , highlands, rilles, and ray craters
B. rilles. Rilles are long, narrow depressions on the Moon's surface that are typically formed by ancient lava flows or tectonic activity. They can appear as cracks in the bedrock when viewed from a distance.
The canyons on the moon are known as rilles. They are thought to have been created by ancient volcanic activity or by the collapse of lava tubes. Rilles can sometimes stretch for hundreds of kilometers across the lunar surface.
# A small brook; a rivulet. # A long narrow straight valley on the moon's surface
The deep narrow valleys on the Moon are called rilles. These are long, winding depressions that can stretch for many kilometers across the lunar surface. Rilles are thought to have been formed by a combination of ancient volcanic activity and tectonic forces.
Cigar-shaped depressions on the Moon are called "rilles." They are long, deep channels that are thought to have been formed by volcanic activity or the collapsing of underground lava tunnels. Rilles can be several kilometers wide and hundreds of kilometers long.
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.
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.