A stratovolcano, also known as a composite volcano.
The cinder cone volcano is named after the type of volcanic material it predominantly emits, known as cinders. These cinders are small, rock fragments that are expelled during eruptions and accumulate around the vent, eventually forming a cone-shaped volcano.
find out your self instead of coming here
A shield volcano forms from repeated eruptions of low-viscosity basaltic lava that flows easily and covers a large area. The lava builds up in layers, gradually creating a broad, gently-sloping volcano with a shield-like shape. These volcanoes are typically not very steep and have a large summit caldera or crater.
Lapilli--Lapilli is pyroclastics the size of walnuts.Cinders-- Cinders are a type of pyroclastic material the size of a pea. According to the text, Earth An Introduction to Physical Geology, Cinders come in different forms when "ejected lava blobs are pulverized by the escaping gases".Blocks-- Blocks are particles larger than Lapilli's and are formed by harden lava.Bombs-- Bombs too help to produce blocks, but they are ejected as lava. They take on an streamline shape. They usually tend to fall on the slopes of a cone volcano and they can be ejected far from the volcano due to the force of escaping gasesI answered this earlier but this is a better answer ;)
A stratovolcano, also known as a composite volcano.
Three different types of volcanoes are: 1) Shield volcanoes; they are large mountains with gentle slopes. 2) Cinder cones volcanoes; they are small volcanoes made of hardened lava chunks called cinders. 3) Composite volcanoes; they are medium sized mountains made up of layers of lava that alternates with cinders.
The cinder cone volcano is named after the type of volcanic material it predominantly emits, known as cinders. These cinders are small, rock fragments that are expelled during eruptions and accumulate around the vent, eventually forming a cone-shaped volcano.
find out your self instead of coming here
A shield volcano forms from repeated eruptions of low-viscosity basaltic lava that flows easily and covers a large area. The lava builds up in layers, gradually creating a broad, gently-sloping volcano with a shield-like shape. These volcanoes are typically not very steep and have a large summit caldera or crater.
Cinder cones are small and steep-sloped, composed of volcanic cinders, and have mildly explosive eruptions. Shield volcanoes are large and shallow-sloped with very runny lava and generally non-explosive eruptions.
1. Cinders (clumps of ash as large from 2 - 64mm.)2. Bombs (blocks of lava that flies through the air along with the ash, these usually fall within 3km[2mm] of a volcano's vents)
No. A shield volcano is a large volcano with broad, shallow slopes formed from layers of lava flows formed by non-explosive eruptions. A cinder cone volcano is a small, steep-sloped volcano composed of pieces of rock formed by lava that was ejected explosively into the air.
a volcano is made of many layers: {| ! colspan="2" | | 1. Large magma chamber 2. Bedrock 3. Conduit (pipe) 4. Base 5. Sill 6. Branch pipe 7. Layers of ash emitted by the volcano 8. Flank 9. Layers of lava emitted by the volcano 10. Throat 11. Parasitic cone 12. Lava flow 13. Vent 14. Crater 15. Ash cloud |}
Lapilli--Lapilli is pyroclastics the size of walnuts.Cinders-- Cinders are a type of pyroclastic material the size of a pea. According to the text, Earth An Introduction to Physical Geology, Cinders come in different forms when "ejected lava blobs are pulverized by the escaping gases".Blocks-- Blocks are particles larger than Lapilli's and are formed by harden lava.Bombs-- Bombs too help to produce blocks, but they are ejected as lava. They take on an streamline shape. They usually tend to fall on the slopes of a cone volcano and they can be ejected far from the volcano due to the force of escaping gasesI answered this earlier but this is a better answer ;)
the Philippines volcano's form thin layer of cooled lava but not really cold like freezing
A stratovolcano is a conical volcano with a steep profile that is composed of many layers of hardened lava, pumice, tephra, and volcanic ash. Stratovolcanoes capable of producing both effusive and explosive eruptions, some of which can be very large. They are the most dangerous type of volcano.