yes it it.....i have proof from my science book from my school. also this rock is formed from existing rocks that is changed by heat, preasure or chemical reactions. also another example of an metamorphic rock is a soap stone which have mostly a gray or black or both color to it.
Hornfels or gneiss are possible metamorphic rock with a greywacke protolith.
Slate, hornfels, schist, gneiss.
Hornfels is a type of rock that is metamorphic. They usually have bands and fine grain, and can come in different colors, such as light gray and dark gray.
Hornfels may be used during construction projects or in the building of roadways. They may also be used as whetstones.
Hornfels is a metamorphic rock formed by the contact between mudstone / shale, or other clay-rich rock, and a hot igneous body, and represents a heat-altered equivalent of the original rock. This process is termed contact metamorphism. Because pressure is not a factor in the formation of hornfels, it lacks the foliation seen in many metamorphic rocks formed under high pressure and temperature regimes. Pre-existing bedding and structure of the parent rock is generally destroyed during the formation of hornfels.
Metamorphic.
Hornfels or gneiss are possible metamorphic rock with a greywacke protolith.
Slate, hornfels, schist, gneiss.
Hornfels is a type of rock that is metamorphic. They usually have bands and fine grain, and can come in different colors, such as light gray and dark gray.
Hornfels may be used during construction projects or in the building of roadways. They may also be used as whetstones.
Hornfels is formed when mudstone or shale come in contact with a hot igneous body and metamorphic rock. This process is called contact metamorphism.
A non-foliated contact metamorphic rock is called a hornfels. Hornfels is called so because of its exceptional toughness and texture both reminiscent of animal horns.
Hornfels is a metamorphic rock formed by the contact between mudstone / shale, or other clay-rich rock, and a hot igneous body, and represents a heat-altered equivalent of the original rock. This process is termed contact metamorphism. Because pressure is not a factor in the formation of hornfels, it lacks the foliation seen in many metamorphic rocks formed under high pressure and temperature regimes. Pre-existing bedding and structure of the parent rock is generally destroyed during the formation of hornfels.
hornfels is a rock or mineral
They are all metamorphic rocks.
Slate, gneiss, skarn, phyllite, hornfels, amphibolite, schist, quartzite, marble, and granulite are all metamorphic rocks.
it is found in Mexico