Igneous Rock

Igneous rocks can weather and erode over time, breaking down into smaller sediment particles. These particles can then be transported by water, wind, or ice, and eventually settle and accumulate in layers. Through compaction and cementation, these layers of sediment can harden into sedimentary rocks.

The cost of igneous rock can vary depending on factors such as quality, size, and location. Generally, smaller pieces may cost between $2-10 per pound, while larger specimens or custom orders could cost hundreds or thousands of dollars. It's best to check with a seller or supplier for specific pricing.

It is igneous because it crystallizes out of cooling magma.

It is intrusive because it can only form deep below ground. The magma cools down very slowly when it is deep below ground and this allows the different minerals that make up granite to grow crystals to sizes big enough that you can see them with the naked eye. If it had cooled fast, like if it was at the surface, then the individual crystals making it up would be super tiny and the resulting rock could not be classified as granite.

Yes, granite is harder than concrete. Granite is a natural stone that is known for its durability and hardness, making it a popular choice for countertops, flooring, and other applications where a strong material is needed. Concrete, while strong and versatile, is generally not as hard as granite.

WD-40 can potentially harm granite surfaces as it contains petroleum-based ingredients that may cause discoloration or damage to the stone over time. It's generally recommended to avoid using WD-40 on granite and instead use a specialized granite cleaner to maintain the stone's appearance and longevity.

Basalt can metamorphose into a rock known as amphibolite. Amphibolite forms when basalt is subjected to high temperatures and pressure, leading to recrystallization of minerals and the development of a new texture.

Yes. It would be intrusive or extrusive depending on whether it cooled slowly--below the surface, or quickly--at or near the surface, from molten rock.

Rhyolite banded is a type of volcanic rock that exhibits alternating light and dark colored bands due to different mineral compositions. These bands form as a result of separate eruptions of lava with varying compositions and temperatures, creating a unique visual pattern in the rock.

Iron has the greatest density, followed by granite, water, and then dry air. Density is the mass per unit volume of a substance, and iron has a higher mass per unit volume compared to granite, water, and dry air.

Well, beneath granite you would find any layer of Mafic igneous rock. Basalt is the most common Mafic rock, so that's a good start. It's what you will typically find forming the ocean floor as well as the heavy layer of the earth's crust beneath the granitic layers.

When magma flows horizontally along rock layers, it can form a feature called a sill. Sills are tabular igneous intrusions that are parallel to the surrounding rock layers. They are typically formed when magma is injected between existing rock layers and cools and solidifies underground.

It takes quite a lot of heat to melt rock, and whatever is melting that rock must loose heat in the process. When molten rock comes out of a volcano, it is closer, in terms of temperature to solidifying than the surrounding rock is to melting. So the lava will cool and harden before the surrounding rock has a chance to melt, especially since the lava is also losing heat to the air. In some cases the surface rock may melt, but in fairly small amounts.

Most rocks with a basaltic composition are typically found in oceanic crust, such as the ocean floors and mid-ocean ridges. Basaltic rocks are also common in volcanic regions like Hawaii and Iceland.

No, basalt is not sialic. Basalt is a mafic rock formed from the rapid cooling of lava, which is rich in minerals like magnesium and iron. Sial, on the other hand, refers to the continental crust, which is composed of lighter silicate minerals like quartz and feldspar.

Holes in igneous rocks are typically formed by gas bubbles getting trapped in the molten rock as it cools and solidifies. These trapped gas bubbles then escape as the rock solidifies, leaving behind cavities or holes.

Granite and gabbro both contain large crystals, but gabbro typically has larger crystals due to its slower cooling rate beneath the Earth's surface compared to granite which cools at or near the surface.

An example of a rock formed by molten material cooling is basalt. Basalt is an igneous rock that typically forms from the cooling of lava at or near the Earth's surface, such as in volcanic eruptions. It has a fine-grained texture and is commonly found in oceanic crust and volcanic islands.

The value of obsidian arrowheads can vary depending on their size, craftsmanship, age, and the market demand. However, typically they are valued for their historical significance and are sought after by collectors and enthusiasts. It's best to consult with a professional appraiser or archaeologist for an accurate assessment of their worth.

Completely molten rock would not contain any crystals. Most magmas, however, are a mixture of molten and solid crystals of some sort. It is possible that a magma could contain larger crystals of a specific mineral.

No, obsidian is not poisonous. It is a naturally occurring volcanic glass that is inert and does not release toxins or harmful chemicals. However, it can have sharp edges that can cause cuts or injuries if not handled carefully.

Granite is a more durable and hard-wearing material compared to limestone, making it better suited for high-traffic areas like doorsteps. Granite is also more resistant to weathering, staining, and scratching, which can help maintain the appearance of the doorstep over time. Additionally, granite has a wider range of colors and textures available, allowing for more design versatility.

The Earth layer that is made of peridotite is the mantle. Peridotite is a type of rock rich in olivine and pyroxene minerals that primarily makes up the upper mantle beneath the Earth's crust.

No, basalt is not an example of a felsic rock. Basalt is an example of a mafic rock, which is rich in iron and magnesium and typically dark in color. Felsic rocks, on the other hand, are rich in silica and aluminum and are lighter in color.

Pillow basalt forms when basaltic lava erupts underwater and cools rapidly, creating pillow-shaped structures. Water cools the lava quickly, causing it to solidify into distinctive pillow-like shapes as it is extruded.

Contact metamorphism is the term that indicates changes in rocks due to the injection of magma. This process occurs when hot magma comes in contact with cooler rocks, leading to changes in mineral composition and texture.