mountain
When a stream cuts into a steep slope, it can create a surface feature known as a gorge or canyon. These formations occur as the water erodes the rock and soil over time, deepening and widening the valley. The steep walls of the gorge are often characterized by exposed rock layers, revealing the geological history of the area.
A narrow valley between hills or mountains, with steep rocky walls and possibly a stream running through
a gourge is a narrow split with steep rocky walls with one that a stream or river runs through hope i helped:) :)
Cirque: A bowl-shaped depression on the side of a mountain, formed by the erosive activity of a glacier. Cirques are typically characterized by steep walls and may contain a small lake called a tarn at their base.
The glacial landform you are referring to is called a "cirque." Cirques are bowl-shaped depressions formed by the erosion of glaciers, typically found at the head of a valley. They often contain a small lake, known as a tarn, and are characterized by steep, rocky walls.
A cirque is a surface feature formed by glaciers that is shaped like an armchair. It is a large bowl-like depression with steep walls carved out by the glacier's erosion.
A deep valley created by the downward cutting of a riverbed is called a gorge. It is typically characterized by steep, rocky walls and can vary in size and depth depending on the erosive power of the river. Gorges are often formed by the continuous erosion caused by the flowing water over time.
A narrow pass between steep heights is called a "gorge" or "canyon." These geological formations are typically characterized by their steep walls and can be formed by erosion from rivers or glaciers over time. Gorges often serve as natural pathways through mountainous terrain.
A canyon with very steep walls is often referred to as a "gorge." Gorges typically feature narrow, deep valleys carved by the erosive action of rivers or glaciers, resulting in dramatic cliffs on either side. These formations can be strikingly beautiful and are commonly found in various landscapes around the world.
This type of geological feature is known as a caldera, formed when the magma chamber beneath a volcano empties, causing the volcano to collapse inward. Calderas can be several kilometers in diameter and are often characterized by steep walls and a flat floor. Examples of calderas include Yellowstone in the United States and Santorini in Greece.
A mountain pass with steep rocky sides is often referred to as a "gorge" or "ravine." These geological formations typically occur in mountainous regions where erosion has carved out a narrow pathway between peaks. The steep walls can make these passes challenging for travel and often create dramatic landscapes. They are significant in both ecological and geological contexts, serving as habitats for various species and providing insight into the Earth's geological history.
Pointed arches is not a feature of Romanesque architecture. Romanesque architecture is characterized by semi-circular arches, thick walls, and small windows. Pointed arches are a signature element of Gothic architecture.