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Although all igneous rocks kind from the solidification of molten material, they deserve to have very different appearances and characteristics depending upon the ingredient of the initial material and where precisely it cooled. Added information about the igneous rock and volcanic landforms displayed in this diagram have the right to be found below.

You are watching: What is a volcanic conduit called after the conduit has solidified and been exposed by erosion?


Introduction

Igneous rocks form from the solidification the once-molten rock material. As soon as this mushy melt is uncovered underground penetrating other rocks, it"s referred to as magma, and the solidified absent is termed intrusive. Through contrast, molten material that has erupted ~ above the Earth"s surface ar is called lava, which cools into what geologists contact extrusive (or volcanic) rocks.

Table of Contents

Lava Flow Lopolith
Fissure Sill
volcanic Neck Stock
volcano Cone Dike
volcano Pipe Laccolith
Magma Chamber Batholith

Because erosion can progressively remove tens of countless feet of rocks overlying intrusive formations, both extrusive and also intrusive rocks can be it was observed on the Earth"s surface, occasionally in nearby proximity. In the diagram above, the dike and also the volcanic neck—despite the latter"s name—are both intrusive features, vice versa, the fissure, lava flows, and volcanic cone are all extrusive.

Because different species of igneous features form under varying conditions, each offers tantalizing clues to the problems under which that solidified.

Some that the most typical igneous features include:

Lava Flow


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An aerial view of a low-silica lava flow seen erupting from Hawaii"s Mauna Loa in 1984. Windy domain picture by RBM, U.S. Geological inspection Hawaiian Volcano Observatory.


Lava Flow

Lava flows are streams that lava that pour out of a volcanic vent or fissure. How quickly lava flows move, and how much they go, counts upon the type of magma that"s erupting. Dark-colored magmas the contain fairly little silica (SiO2), choose those it was observed in Hawaii, have the right to travel further and faster 보다 light-colored magmas, which tend to be much stickier. Lava flows deserve to be really destructive, burying and burning everything in their paths.

Geologists likewise use the term lava flow to describe the rock that eventually solidifies from the flowing, molten lava. Basalt is an instance of one extrusive igneous rock formed from dark-colored lava. Rhyolite is an example of an extrusive igneous rock formed from light-colored lava.

Fissure


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Fissure

A lengthy crack top top the Earth"s surface from i m sorry lava pours the end is referred to as a fissure. This kind of volcanic activity is referred to as a "fissure eruption". That most frequently occurs in places where dark magmas through low silica materials erupt, such together the Holuhraun lava areas of Iceland and Kilauea Volcano of Hawaii.

Volcanic Neck


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Volcanic Neck

This landform, i m sorry is additionally called a volcano plug, is produced when magma solidifies inside a conduit causing a volcano or a volcano vent. Since the resulting absent is frequently harder 보다 the product it intrudes into, it"s left standing after the surrounding, softer rock has eroded away. This attribute is as such often dubbed the "throat" the a volcano. A classic example is ship Rock, a volcanic neck top top the Navajo Reservation the rises nearly 1,600 feet above the desert near Farmington, brand-new Mexico.

Although the usage of "volcanic" in the name argues that volcanic necks space extrusive features, they are made up of intrusive igneous rocks.

Volcanic Cone


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Sunset Crater, a 1,000-foot-high volcano cone in north Arizona, is the centerpiece the Sunset Crater nationwide Monument. Public domain photo by the nationwide Park Service.


Volcanic Cone

Volcanic cones are steep-sided hills or mountains built of class of erupted lava flows and also fragments of volcano rocks that have actually piled up about a main vent. As the name suggests, these features tend to be conical in shape and can it is in light- or dark-colored. There room three species of volcano cones: 1) cinder cones, composite cones, and also shield volcanoes.

Sunset Crater in north Arizona is an instance of a cinder cone so young that neighborhood farmers nearly surely watched it erupt around 900 years ago.

Volcanic Pipe


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The main conduit v which magma rises in a volcano is called a volcano pipe.


Volcanic Pipe

A volcano pipe is a vertical conduit beneath a volcano with which magma when passed ~ above its journey from the magma chamber to the eruption site. End time, volcano pipes usually come to be clogged by coagulation magma and also other volcano rocks, leaving a hard, cylindrical-shaped formation behind. These attributes can selection in broad from number of yards to approximately half a mile.

Magma Chamber


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Areas whereby molten rock product pools underground are dubbed magma chambers. They deserve to be the source of both extrusive and also intrusive igneous rocks.


Magma Chamber

A magma room is a pool of molten absent material situated beneath the Earth"s surface. Over lengthy periods the time, magma chambers can crystallize into big intrusive igneous rock formations referred to as batholiths. Magma chambers can be the source of both magma and lava.

An inactive magma chamber will cool progressively over time. This sluggish cooling enables the magma come crystallize into a coarse-grained igneous rock. Granite, gabbro, and also diorite are instances of rocks that can type during the crystallization of a magma chamber.


Lopolith


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Lopoliths space intrusions the igneous rocks with bowl-shaped floors and also either level or bowl-shaped tops.


Lopolith

A lopolith is a large, layered igneous intrusion that is identified by the convex-downward bowl shape of that is floor and whose top deserve to either be flat or convex down.

Sill


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The sill close to the peak of Colorado’s technician Mountain displays vertical cracks thatformed as this igneous rock cooled. Photo by Daniel Weber.


Sill

A sill is a flat, sheet-like igneous rock mass that forms when magma intrudes into and crystallizes between preexisting absent layers. Sills can kind from magmas through a selection of silica contents. These attributes can vary from less than one customs up to thousands of feet thick and can prolong for many miles.

The tabular massive of quartz trachyte close to the summit that Engineer mountain near Silverton, Colorado is a well-known example of a sill.

Stock


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Stocks are tiny igneous intrusions with less than 40 square miles exposed at the Earth"s surface.


Stock

A relatively small igneous intrusion that forms when magma crystallizes underground. Although uplift and/or erosion have the right to later unearth component of a stock, this feature is defined as having less than 40 square mile (100 square kilometers) exposed at the surface.


Dike


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Dike

A tabular igneous intrusion that crosses through various other (layered or non-layered) rocks at a steep angle. Dikes can happen alone or in sets and may be made up of irradiate (high-silica) or dark (low-silica) rocks, or any kind of composition in between. One of the most-photographed examples originates from the grand Canyon, whereby a dark dike slashes throughout thin, red shale layers above a frothing whitewater rapid.

Laccolith


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Dark host rocks overlie the light-colored, intrusive igneous spires the the Torres del Paine massif, i beg your pardon glaciers sculpted from a 12.6-million-year-old laccolith. Credit: Terri Cook and Lon Abbott.


Laccolith

Laccoliths are intrusive igneous rock formations distinguished by your characteristic lens shapes. These features kind when the pressure of the magma intruding between preexisting layers causes the overlying rocks to dome up, developing a mushroom shape. Among the world"s most spectacular examples of a laccolith is discovered in Chile"s Torres del Paine nationwide Park.

Batholith


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Batholith

A relatively big igneous intrusion that forms when magma crystallizes underground and also is later partially exposed complying with uplift and/or erosion. By definition, batholiths have much more than 40 square miles (100 square kilometers) of surface exposure. The love of California"s Sierra Nevada mountains is sculpted from a granitic batholith emplaced between about 120 and 85 million years ago.

About the Author: Terri Cook

Growing up in a residence whose cornerstone to be a meteorite inspired Terri to end up being an award-winning travel and science writer. A geologist by training and also a member of both the society of American travel Writers and the nationwide Association of science Writers, Terri weaves accurate, engaging story for a wide variety of clients and also outlets including the U.S. Geological Survey, Eos, clinical American, and also Lonely Planet. Terri is additionally the writer or co-author of five books, consisting of Hiking the grand Canyon’s invernessgangshow.net, invernessgangshow.net Underfoot in northern Arizona, and invernessgangshow.net Underfoot follow me Colorado’s front Range. She is a 2019 association of Health care Journalists Fellow, a 2016 EGU science Journalism Fellow, and the 2019-2020 Science interaction Fellow for the Geological society of America.


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