Volcanic necks consist of plutonic rock formed during eruptions. Plutonic rocks actually cool below the surface, so they have more time to form stronger bonds and as such last longer than the ejected material.
Imagine a nearly flat surface as the volcano erupts the first time. The ground is pushed up as the magma rises to the surface. Rock is pretty hard, so typically magma is only ejected in relatively small areas (caldera forming eruptions are the exception). As it does this, it forms a tube, of sorts, which allows the magma to flow upward easier and the end result, after numerous eruptions, is a mountain.
While the volcanic rock (ash, glass, etc.) forms the outer slopes of the newly formed mountain, the stronger rock lies inside the slopes, forming the neck.
Fast forward a few million years: Erosion has taken place, removing the less resistant rock away, and leaving the volcanic neck, renamed a butte, behind.
Because volcanic necks have a lot of magma flowing through them, they can be a hodgepodge of different minerals, such as diamonds, emeralds, etc, in a kimberlite matrix.
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When magma hardens in a volcano's pipe, the result will eventually be a volcanic neck or volcanic plug. This landform is a solidified remnant of magma that once filled the volcano's vent.
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Volcanic Neck The surrounding rock weathers more easily than the magma in the pipe. The resultant structure will first appear as a low flat protrusion which is slightly elevated from its surroundings. With additional weathering of the surrounding rock, the hardened magma may appear as a tower with possible basaltic columnar structure known as a volcanic plug or volcanic neck.
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A volcanic conduit that has solidified and been exposed by erosion is called a volcanic neck or volcanic plug. These features are made up of solidified magma that once flowed through the conduit of a volcano.
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