Cinder cone
A volcanic feature that fits this description is a volcanic cone. It is a tall, narrow mountain formed around a vent with steep sides as a result of the accumulation of lava, ash, and other volcanic materials ejected during eruptions.
Isolated volcanic peaks on the ocean floor are known as seamounts. The deepest parts of the ocean are long, narrow features known as deep ocean trenches.
The mountain is likely a young mountain, formed relatively recently in geological terms due to tectonic forces pushing the Earth's crust upward. The steep sides, sharp peaks, and narrow valleys are characteristic features of young, rugged mountains that have not been eroded much by weathering and other natural processes yet. Over time, the mountain will likely experience erosion that softens its features and changes its landscape.
A tall, narrow rock formed from wave erosion is known as a sea stack. Sea stacks are created when the relentless force of ocean waves erodes the softer rock around a more resistant single column of rock, eventually isolating it from the mainland.
cataract
A volcanic feature that fits this description is a volcanic cone. It is a tall, narrow mountain formed around a vent with steep sides as a result of the accumulation of lava, ash, and other volcanic materials ejected during eruptions.
A volcanic mountain with a narrow base and steep sides is typically called a volcanic cone or a cinder cone. These cones are formed from explosive eruptions that eject mostly tephra and volcanic ash, resulting in their characteristic steep shape.
A mountain gully is often referred to as a ravine. It is a deep, narrow valley with steep sides, typically formed by running water erosion.
A narrow gap through a mountain range is called a mountain pass. These passes are also sometimes known as gaps, saddles, and cols.
A long narrow chain of hills and mountains is called a mountain range or a mountain chain.
A five-letter word for "narrow mountain stream" is "brook".
Maria: Large, dark, flat areas formed by ancient volcanic eruptions. Craters: Bowl-shaped depressions created by asteroid or comet impacts. Rilles: Long, narrow valleys likely formed by ancient volcanic activity. Highlands: Bright, rugged, mountainous areas composed of older lunar crust. Lunar domes: Small, rounded hills formed by volcanic activity.
The narrow zone on the mid-ocean ridge crest where most geologic activity occurs is called the rift zone. It is characterized by high heat flow, volcanic eruptions, and tectonic spreading, creating new oceanic crust as magma rises to the surface and solidifies.
young
Stack is a tall narrow rock formed from was erosion.
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.
Isolated volcanic peaks on the ocean floor are known as seamounts. The deepest parts of the ocean are long, narrow features known as deep ocean trenches.