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A geyser is a hot spring that periodically erupts hot water and steam, while a volcano is a mountain that erupts molten rock, ash, and gases. Geysers are formed by underground water heated by magma, while volcanoes are formed by the movement of tectonic plates. Geysers erupt due to pressure build-up in underground chambers, while volcanoes erupt due to the release of pressure from molten rock.

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Compare the formation of Hawaii with that of paricutin?

Hawaii formed as a result of a hot spot volcanic activity over a stationary tectonic plate, leading to a chain of islands. Paricutin formed as a result of a single eruption in a continental crust, creating a cinder cone volcano. Both are examples of volcanic formations, but the mechanisms and processes of their formation differ.


How did it effect the environment of MT Vesuvious?

The eruption of Mount Vesuvius in 79 AD caused widespread destruction of the surrounding environment, covering nearby cities like Pompeii and Herculaneum in volcanic ash and pumice. The eruption also led to the loss of agriculture and vegetation in the region. Additionally, the volcanic activity altered the landscape and created new geological formations in the area.


When was mt shastas last eruption?

Mount Shasta's last known eruption occurred around 1786, based on geological records. Since then, the volcano has been classified as dormant, with no recent signs of volcanic activity.


What is emplacement mechanism?

Emplacement mechanism refers to the process by which igneous rocks are created and placed into their final position within the Earth's crust. This can involve various mechanisms such as magmatic intrusion, volcanic eruption, or solidification of magma underground. Emplacement mechanisms play a key role in understanding the formation and distribution of igneous rocks.


Some examples of geological processes are?

Geological processes are processes that shape or change the physical makeup of the planet. If you think about it you will realize that things like erosions, earthquakes, and meteor impact change the earth which makes them geological processes. (:

Related Questions

What happens when there is a geological change?

When there is a geological change, such as an earthquake or volcano eruption, it can cause shifts in the Earth's surface, leading to things like landslides, tsunamis, or the formation of new land formations. These changes can have both short-term and long-term impacts on the environment and ecosystem.


Describe why a terrain has a different geologic history from that of the surrounding area?

A terrain may have a different geologic history due to variations in processes such as erosion, sedimentation, volcanic activity, or tectonic movements that have occurred over time. Localized events, like a volcanic eruption or an earthquake, can dramatically alter the landscape and its geological features, creating distinct formations. Additionally, factors like climate, water flow, and biological activity can influence the rate and type of geological changes, leading to divergent histories. These differences contribute to the unique geological characteristics of the terrain compared to its surroundings.


What is a pinion eruption?

A pinion eruption refers to a specific type of volcanic activity characterized by the explosive release of gas and magma, resulting in the formation of a pinion-like structure. This term is often used in the context of certain types of eruptions that produce distinct, spire-like formations due to the rapid expulsion of volcanic material. These eruptions can create unique geological features and are typically associated with stratovolcanoes. The term "pinion" itself can also refer to the shape and structure of the resulting formations, resembling the pointed end of a pinion gear.


What are the two main transport mechanisms of lava?

The two main transport mechanisms of lava are flow and explosive eruption. Lava can flow steadily like a river, known as effusive eruption, or it can be ejected violently into the air during explosive eruptions. Both mechanisms depend on factors such as lava viscosity, gas content, and eruption style.


What margin does Eyjafjallajokull iceland have?

Eyjafjallajökull, the famous volcano in Iceland, has a margin characterized by its position along the Mid-Atlantic Ridge, where the North American and Eurasian tectonic plates diverge. This geological setting contributes to the volcano's frequent activity and unique eruptions, including the significant 2010 eruption that disrupted air travel across Europe. The surrounding glaciers and geological formations further define its striking landscape.


What are the names of the different types of volcano formations?

The main types of volcano formations are shield volcanoes, stratovolcanoes (composite volcanoes), cinder cone volcanoes, and calderas. Each type has distinct characteristics based on their eruption style and the type of materials they release.


When was mount vesuvius's first eruption?

79 AD


What is an accurate statement about volcanoes?

Volcanoes are geological formations where molten rock, gases, and ash erupt from beneath the Earth's crust. They can be classified into different types, such as shield, stratovolcano, and cinder cone, based on their shape and eruption style. Volcanoes play a crucial role in shaping landscapes and can also impact climate and ecosystems through their eruptions. Additionally, they are often found at tectonic plate boundaries, where plates converge or diverge.


What is mapping in geology?

Geological mapping is the production of a map containing the areal extent of outcrops of different types of rocks, their geometric relations to each other and partly also their internal structure. Depending on which types of rocks are most abundant (igenous, metamorphic or sedimentary), different mapping strategies may be employed. Usually formations are assigned which are packages of strata that are easy to distinguish from other rocks and form a coherent complex (similar depositional environment, similar facies, same volcanic eruption, same degree of metamophic overprint etc.) These formations and especially the boundaries between two formations are than followed in the field and the structural (dip, plunge, shear indicators etc.) as well as lithological (composition) information is stored in a map. From the information derived from the mapping of outcropping rocks a geological profile is constructed (this is always the case for a real geological map). The profile section is drawn along a relevant line (according to the purpose of the map) and shows how the strata that were found on the surface continue in the subsurface. Often this sub-surface information is what makes geological maps a precious tool for companies and scientists as one can predict, where certain rocks (and ressources) can be found.


Does Santorini classify as a volcano?

Yes, Santorini is a volcanic island known for its geological formations created by past volcanic activity. The island's main feature is the caldera, a large submerged volcanic crater, which was formed by a massive volcanic eruption in the Bronze Age.


Openings in Earth and crust that allow magma to reach the surface is called .?

Openings in the Earth and crust that allow magma to reach the surface are called volcanoes. These geological formations can erupt, releasing lava, ash, and gases. Volcanoes can vary in size and type, including shield, stratovolcano, and cinder cone, depending on their eruption styles and materials.


What are the 4 types of mafic lava?

The four types of mafic lava are basalt, basaltic andesite, hawaiite, and mugearite. Basalt is the most common, characterized by its low viscosity and rapid flow. Basaltic andesite contains a higher silica content, while hawaiite and mugearite have increasing amounts of alkalis and are typically found in the Hawaiian Islands. Each type exhibits different mineral compositions and eruption styles, impacting their geological formations.