Moraine
Where cirques intersect is called a "paternoster lake." These lakes form in a series of depressions created by glacial erosion, typically found in mountainous regions. As cirques erode, they can create multiple basins that fill with water, resulting in a chain of lakes. Paternoster lakes are named for their resemblance to a rosary, with beads (lakes) strung along a chain (the valley).
Opposite sides are congruent Opposite sides are parallel Opposite angles are equal Consecutive angles are supplementary Diagonals bisect each other Diagonals form 2 equal triangles
Not always. You could form a kite. That means that the two adjacent sides would be congruent, not the two opposite sides.
constructive interference
Symmetry is the exact correspondence of form and constituent configuration on opposite sides of a dividing line or plane or about a center or an axis.
this is a peproduction
Glaciers that create cirques on the sides of mountains are called cirque glaciers. These glaciers form in bowl-shaped depressions on the slopes of mountains and are responsible for eroding and shaping the characteristic amphitheater-like features known as cirques. Examples of cirque glaciers can be found in mountain ranges around the world, such as the Alps, Andes, and Himalayas.
Cirques and U-shaped valleys are formed by glacial erosion. Cirques are formed by the erosive action of a glacier in a bowl-shaped depression at the head of a valley. U-shaped valleys are carved out by glaciers as they flow down a mountain, eroding the surrounding rock and creating a distinctive U-shape.
Deglaciation is not a feature associated with valley glaciers. Valley glaciers form in mountainous regions due to the accumulation and compaction of snow, creating a flowing mass of ice within a valley. Features associated with valley glaciers include cirques, arêtes, and moraines.
Where cirques intersect is called a "paternoster lake." These lakes form in a series of depressions created by glacial erosion, typically found in mountainous regions. As cirques erode, they can create multiple basins that fill with water, resulting in a chain of lakes. Paternoster lakes are named for their resemblance to a rosary, with beads (lakes) strung along a chain (the valley).
The general form is a rhombus.
Cirques could intersect at an intermediate ridge. This would be less common.
That's a trapezium, a form of irregular quadrilateral.
A hanging valley forms when a smaller glacier flows into a larger glacier, leaving the smaller valley elevated above the main valley floor after the larger glacier retreats. A cirque is created by the erosion of a mountain side by a glacier, resulting in a bowl-shaped depression. An arete is a sharp ridge formed between two cirques that erode toward each other. A horn is a pointed mountain peak that results from the glacial erosion of multiple cirques surrounding a summit, sharpening it into a distinctive shape.
Answer: Cirques
The hypotenuse is the side opposite the two sides that form a right angle.
Opposite sides are congruent Opposite sides are parallel Opposite angles are equal Consecutive angles are supplementary Diagonals bisect each other Diagonals form 2 equal triangles