Long narrow valleys on the Moon's surface are known as "rilles." These geological features, which can be several kilometers wide and hundreds of kilometers long, are typically formed by volcanic activity or the collapse of lava tubes. Rilles can be classified into two main types: sinuous rilles, which have a winding, river-like appearance, and straight rilles, which are more linear. Their presence provides insight into the Moon's volcanic history and tectonic processes.
Those features are called rilles, which are long, narrow valleys on the surface of the Moon. They can be several kilometers wide and hundreds of kilometers long, and are thought to have been formed by ancient lava flows or tectonic activity.
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.
These are called lunar rilles, which are long, winding valleys on the Moon's surface. They are thought to have formed from a combination of processes such as ancient volcanic activity and tectonic forces.
Rilles. Rilles are long, narrow depressions on the Moon's surface, often found in lunar maria. They can be several kilometers wide and hundreds of kilometers long, thought to have been formed by ancient lava flows or collapsing lava tubes.
The valleys on the moon are called rilles. They are long, slender depressions that may have curved or twisting shapes. They may be caused by collapsed lava tubes, cooling lava flows, or parallel crustal faults.
Those features are called rilles, which are long, narrow valleys on the surface of the Moon. They can be several kilometers wide and hundreds of kilometers long, and are thought to have been formed by ancient lava flows or tectonic activity.
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.
These are called lunar rilles, which are long, winding valleys on the Moon's surface. They are thought to have formed from a combination of processes such as ancient volcanic activity and tectonic forces.
trenches
trenches
Long valleys or trenches associated with lunar maria are called "rilles." These features are formed by ancient volcanic activity or the collapse of surface materials, creating narrow, elongated depressions. Rilles can vary in size and shape, ranging from straight to meandering paths across the lunar 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.
rille
I don't
There are more than one term for a deep narrow valley. Glens, canyons, ravines, fjords are terms you could use.
A long narrow mark could be a scratch on a surface, a streak of light, or a thin line drawn with a writing implement.
from volcanos that were on the moons surface long ago