Yes, they are.
Actually, a volcanic mountain with a wide base and gently sloping sides is called a shield volcano. Shield volcanoes are typically formed by low-viscosity lava flows that spread out in layers, creating a broad, shield-like shape.
Actually, a volcanic mountain with gently sloping sides made of basalt lava flows is typically called a shield volcano, not a cinder cone. Cinder cones are typically smaller, steeper-sided volcanoes formed from ejected rock fragments.
A volcanic mountain with a wide base and gently sloping sides is called a shield volcano. These types of volcanoes are characterized by their low profile and are formed by the slow and steady accumulation of lava flows. They can be found in areas with hot spots or along divergent plate boundaries.
A parasitic cone is a small volcanic cone that forms on the flanks of a larger volcano. These cones are usually aligned with the main vent and form as a result of secondary eruptions of lava and ash from separate vents on the volcano's slope. They are often temporary features that can become inactive once the main volcano stops erupting.
Mauna Kea is a shield volcano, which is a type of volcano with gentle sloping sides caused by basaltic lava flows. It is known as a dormant volcano, last erupting about 4,500 years ago.
The sides of a volcano are known as flanks.
yes it is called a flanks.
It is called a side vent.
The Stratovolcano is. It can reach into the stratosphere. Cinder cones are usually formed on the flanks or sides of shield or stratovolcanos. See the related links for further information.
It is a shield volcano. Rifts typically open in the seaward flanks, with lava fountains and slow-moving lava flows to the ocean.
The flank of a volcano is the ridge at the top opening of the volcano that was created by lava deposits during eruption,æ Volcano flanks are very unstable and can contain vertical fractures which make them dangerous to study.
A shield volcano most commonly found at hot-spots and island chains such as Hawaii they have shallow flanks, a wide base, and runny lava which is frequently erupted, so it is non-explosive because there is little pressure build up
A shield volcano is broad with gently sloping sides.
Shield Volcano.
A broad volcano with gently sloping sides describes a shield volcano. These types of volcanoes are characterized by their low, wide profile and are formed by the slow accumulation of fluid lava flows over time, which create a shield-like shape. This type of volcano tends to have non-explosive eruptions due to the low viscosity of the lava.
The flanks/outer edge of the fire from both sides
sheild volcano