shield volcano
it is a shield volcano
a shield volcano
This is called a shield volcano and an example would be Hawaii.
The type of volcano is the shield volcano. Shield volcanoes can be found in Hawai'i.
Shield volcanoes typically have gentle slopes with angles ranging from 2-10 degrees. These low-angle slopes are a result of the highly fluid lava flows produced by shield volcanoes, which travel long distances before solidifying. This gradual build-up of lava layers over time creates the characteristic broad, dome-like shape of shield volcanoes.
A shield volcano has very broad, gentle slopes.
It is likely a shield volcano, which is formed by the accumulation of numerous low viscosity lava flows. These volcanoes have gentle slopes due to the runny nature of their lava, allowing it to spread out widely as it flows. Examples of shield volcanoes include Mauna Loa in Hawaii and Mauna Kea.
A low, wide-based volcano is called a shield volcano. These types of volcanoes have gentle slopes and are formed by the gradual flow of low-viscosity lava. Examples include Mauna Loa in Hawaii and Iceland's shield volcanoes.
Kohala Volcano, located on the Big Island of Hawaii, was formed through a series of volcanic eruptions over approximately a million years. It is considered a shield volcano, characterized by its broad, gentle slopes created by the eruption of low-viscosity basalt lava. Kohala is the oldest of the five volcanoes on the island and became dormant around 120,000 years ago, with its last eruptions occurring about 60,000 years ago. The volcano's formation is primarily due to the movement of the Pacific tectonic plate over a stationary hotspot in the Earth's mantle.
A shield volcano is a roundish, moundlike volcanic cone with very gentle slopes.
The kind of mountain you are describing is most likely a "gentle sloping mountain" or a "shield volcano." These mountains are formed by layers of hardened lava flows and have weathered over time to have rounded peaks and gentle slopes. They are typically found in areas of low volcanic activity.
Mount Tambora is not a shield volcano; it is a stratovolcano. Stratovolcanoes are characterized by steep slopes and a symmetrical shape due to their alternating layers of lava, ash, and other volcanic materials. Shield volcanoes, on the other hand, have gentle slopes and wide bases formed by successive layers of flowing lava.