Metamorphic Rock

Metamorphic rock is generally denser than sedimentary rock. This is because metamorphic rocks undergo intense pressure and/or heat, which causes the minerals within them to recrystallize and become more tightly packed, resulting in a denser structure. Sedimentary rocks, on the other hand, are formed from the accumulation and compression of loose sediment particles, which may not be as dense as the tightly packed minerals in metamorphic rocks.

Fluorite is a mineral, not a rock, and it is not metamorphic. Fluorite is a common mineral that can be found in a variety of rock types, including igneous and sedimentary rocks. It forms through a variety of processes, such as hydrothermal deposition and precipitation from groundwater.

Marble chips are made of limestone that has undergone metamorphism, resulting in a crystalline structure. They are composed primarily of calcium carbonate and are often used in landscaping and construction for their decorative and functional properties.

Slate countertops are not completely heat-proof. While slate is heat resistant to an extent and can handle hot pots and pans, extreme heat or prolonged exposure to high temperatures can still damage the surface by causing cracks or discoloration. It is always advisable to use trivets or hot pads to protect the surface from direct heat.

Schist rocks can be both permeable and impermeable, depending on factors such as the size and arrangement of mineral grains, the presence of fractures or faults, and the level of metamorphism they have undergone. In general, schist rocks tend to have higher permeability compared to other metamorphic rocks such as gneiss or marble.

Metamorphic rocks change due to high temperature and pressure deep within the Earth's crust. These conditions cause the minerals within the rock to recrystallize, resulting in a new texture and sometimes new minerals forming. Additionally, the presence of fluids can also contribute to the chemical changes that occur during metamorphism.

The layer of the Earth that fits this description is the continental crust. It is the outermost layer of the Earth and is primarily composed of granite and gneiss rocks. The continental crust is thicker and less dense compared to the oceanic crust.

Hornfels rocks are typically found in areas where there has been high heat and pressure, such as near igneous intrusions or along fault zones. They are commonly found in regions with a history of regional metamorphism, such as mountain ranges or areas near tectonic plate boundaries.

Quartzite is often referred to as "quartzite rock" or simply "quartzite." It is a metamorphic rock that is composed primarily of quartz grains.

The metamorphic rock commonly found in a pencil is graphite. Graphite is a soft, black mineral that forms from the metamorphism of carbon-rich sediments. It is composed of layers of carbon atoms arranged in a hexagonal pattern.

Marble and quartzite are examples of massive metamorphic rocks that lack banding. Marble is formed from the metamorphism of limestone, while quartzite is formed from the metamorphism of sandstone. Both rocks typically have a uniform composition and lack the distinct layering or banding that is characteristic of other metamorphic rocks.

Michelangelo used Carrara marble, which is a type of metamorphic rock, to create famous sculptures such as David and Pieta. Carrara marble is known for its white color and fine, even texture, making it a popular choice for sculptors throughout history.

Igneous rocks and metamorphic rocks both form within the Earth's crust. They are both created through the process of solidification, although igneous rocks solidify from molten magma while metamorphic rocks form from the alteration of existing rocks through heat and pressure. Both types of rocks can be found in a wide range of geological settings.

Yes, foliated metamorphic rocks tend to break along their layers or foliation planes due to the alignment of minerals during metamorphism. This can result in the rock breaking into thin sheets along its outer edges.

The protolith for greenstone is usually basaltic or andesitic volcanic rock that has undergone metamorphism, resulting in the formation of chlorite, epidote, and actinolite minerals that give greenstone its characteristic green color. These rocks are typically found in greenschist facies metamorphic environments.

a sedimentary rock,

a sedimentary rock is one that has sediments or minerals that create layers this rock is

formed when preasure is put upon it.

Anthracite fractures conchodially. The fractures resemble small half circle pockets.

Depends on which one. Diamond is a metamorphosed coal/carbon that is the hardest natural substance known. Marble is metamorphosed limestone that is much softer. It's safe to say that all metamorphosed rocks are harder than they were in their pre-metamorphosed form.

Metamorphic rocks are nonexistent in central and Eastern England. Good places are hilly regions where rocks have been deformed by tectonic collisions. The best places for this are the Scottish-English border, Cornwall and Western Devon.

I recommend the free smart phone app 'iGeology' from the British Geological Survey for more information.

Sandstone can be metamorphosed into quartzite. Heat and pressure bake the sandstone and it becomes extremely hard.

According to 118 118, metamorphic rocks make up about 85% of the earth's Continental crust.

According to wiki.answers, 75-80% of the earth's surface is composed of sedimentary rock. 20-25% left to be composed of igneous and metamorphic rock.

Change over large areas - usually the deeper down rocks are the more change occurs.Usually due to both heat and pressure.Mountain Ranges are example of large area metamorphic.

Change over small areas - formed by heat pressure ALONE

An organic metamorphic rock, also known as biogenic, is composed of materials from the activities of living organisms. Coal, which is formed from undecayed compacted plant matter from ancient swamps, and Limestone, which is formed from deposits of shells or skeletal fragments that collect at the bottom of the ocean are examples of organic metamorphic rock.

The Blank Slate theory believes that each person is like a blank slate when born ie no innate characteristics separate from environment. This means that each person is defined by their environment.