dome
Conical hills are landforms that have a rounded, cone-shaped appearance, usually formed by the erosion and weathering of softer rock layers surrounding a harder core. They are often found in areas with sedimentary rock and can vary in size from small mounds to prominent peaks. Conical hills are a common feature in landscapes shaped by natural processes such as wind, water, and glaciation.
cinder cone volcanoes: consist of primarily erupted volcanic ash and rock fragments, or cinders. When the volcano erupts the ash and rock are ejected onto the mountain. As this process continues the volcano "grows" higher because of the debris build up.
a cinder cone volcanoe looks like a ant hill
drumlin
Which is a cone-shaped hill or small mountain.
Which is a cone-shaped hill or small mountain.
Which is a cone-shaped hill or small mountain.
Composite Volcanoes!
Ash, cinder and bombs erupt explosively to form a cone shaped hill
Magma burst on to the surface of earth,when it dries, they will form a large hill of rocks sky as it develops the hill becomes a volcano .
A cone shaped hill or mountain is often created by volcanic activity, where hardened lava forms the steep, conical shape. These features can be found in volcanic regions around the world, such as Mount Fuji in Japan or Mount Kilimanjaro in Tanzania. The symmetrical cone shape is a result of the build-up of lava and ash over time.
dome
Puy - a cone shaped hill that is the remains of an extinct volcano - is a noun and so doesn't have a past tense. Only verbs have a past tense.
Conical hills are landforms that have a rounded, cone-shaped appearance, usually formed by the erosion and weathering of softer rock layers surrounding a harder core. They are often found in areas with sedimentary rock and can vary in size from small mounds to prominent peaks. Conical hills are a common feature in landscapes shaped by natural processes such as wind, water, and glaciation.
cinder cone volcanoes: consist of primarily erupted volcanic ash and rock fragments, or cinders. When the volcano erupts the ash and rock are ejected onto the mountain. As this process continues the volcano "grows" higher because of the debris build up.
A cinder cone is formed when a very gassy magma erupts, it is a steep conical hill of loose pyroclastic fragments (volcanic clinkers, cinders, volcanic ash) called scoria.The explosive eruptions or lava fountains occur from single, typically cylindrical, vents and as the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as scoria around the vent to form a cone that often is beautifully symmetrical; with slopes between 30-40° with a bowl shaped depression at the top.