A spatter cone is formed of molten lava ejected from a vent of a volcano. Expanding gases in the lava fountains tear the liquid rock into irregular gobs that fall back to earth, forming a heap around the vent. The partly liquid rock splashes down and over the sides of the developing mound is called spatter. Because spatter is not fully solid when it lands, the individual deposits are irregular in shape and weld together as they cool, and in this way differ from cinder and ash. A cinder cone is a volcanic cone built almost entirely of loose volcanic fragments called cinders. They are built from particles and blobs of congealed lava ejected from a single vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as cinders around the vent to form a circular or oval cone. Most cinder cones have a bowl-shaped crater at the summit.
Cinder cones are formed from fragmented lava ejected from a single vent, typically consisting of volcanic rock fragments. Spatter cones are built from blobs of molten lava that are ejected from a vent and solidify into volcanic rock. In essence, cinder cones are made of solidified volcanic fragments, while spatter cones are formed from solidified lava droplets.
Yes, cinder cones can produce lava flows. Typically, these flows are relatively short and are composed of basaltic lava. Cinder cones are formed from the accumulation of volcanic cinders and ash around a central vent.
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.
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 cinder cone volcano is built almost entirely from ejected lava fragments. These fragments can range in size from ash to bombs and are ejected during explosive eruptions. Over time, these layers of eruptive material accumulate to form a steep-sided cone-shaped volcano.
Plinian, Strombolian and Hawaiian..:P
Cinder Cones, and Spatter Cones +Ang ganda ko :)
3 3 Five: Shield, Composite/Strato, Cinder Cones, Spatter Cones and Complex.
5, Composite (strato), Shield, Cinder Cones, Spatter Cones and Complex Volcanoes
their are 6 cinder cone volcanes
Cinder cones generally have a very steep slope. This slope is also considered gentle compared to the cones' short height.
Cinder Cones are composed of rock fragments and the eruption of cinders. The rock fragments pile up around a single crater forming a Cinder Cone.
explosive
no
yes
explosive
No. Cinder cones are formed by basaltic magma.
Cinder cone volcanoes erupt explosivly.