Which of the following textures indicates two stages of cooling and crystallization?

The texture of an igneous rock is determined by the cooling history of the magma from which it formed. … Phaneritic texture describes coarse grained rocks. They are characteristic of intrusive (plutonic) rocks and have crystals that can be seen with the unaided eye. Indicates slow cooling history.

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What are the textures of an igneous rock tells us about cooling history?

Extrusive or volcanic rocks crystallize from lava at the earth’s surface. The texture of an igneous rock (fine-grained vs coarse-grained) is dependent on the rate of cooling of the melt: slow cooling allows large crystals to form fast cooling yields small crystals.

What does the porphyritic texture tell you about the cooling history of the magma?

This porphyritic texture indicates that the magma sat and cooled a bit below the Earth’s surface thus giving time for the large crystals to grow before erupting onto the surface and cooling very quickly.

What rocks cool when magma cools?

Igneous rocks form when magma (molten rock) cools and crystallizes either at volcanoes on the surface of the Earth or while the melted rock is still inside the crust.

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How does the cooling time of the magma affect the texture?

If the magma cools quickly the crystals do not have much time to form so they are very small. If the magma cools slowly then the crystals have enough time to grow and become large. … And some magma cools so quickly that no crystals form we say that these have a hyaline texture (from the Greek “hyalis” meaning glass).

What do igneous rock textures say about the rock that formed?

The igneous texture tells us how the magma cooled and solidified. Magma can solidify into igneous rock in several different ways each way resulting in a different igneous texture. Magma may stay within the earth far below ground level and crystallize into plutonic igneous rock (also known as intrusive igneous rock).

How would you describe the texture of this igneous rock?

Plutonic Rocks

The texture of an igneous rock made up entirely of crystals big enough to be easily seen with the naked eye is phaneritic. Phaneritic texture is sometimes referred to as coarse-grained igneous texture. Granite the most well known example of an intrusive igneous rock has a phaneritic texture.

What does a porphyritic texture indicate about the history of igneous rock?

What does a porphyritic texture indicate about the cooling history of an igneous rock? It indicates that crystals were formed at depth (slow cooling) and then the magma moved to a shallow depth or erupted (fast cooling).

What does a porphyritic texture mean?

Porphyritic – This texture describes a rock that has well-formed crystals visible to the naked eye called phenocrysts set in a very fine grained or glassy matrix called the groundmass.

What is a porphyritic texture How do you think porphyry are created?

Most igneous rocks have some degree of porphyritic texture. This is because most magma from which igneous rock solidifies is produced by partial melting of a mixture of different minerals.

What is cooling magma?

Magma is molten rock material. As magma cools the elements within the magma combine and crystalize into minerals that form an igneous rock. Magma cools either below the surface or at the surface (magma that reaches the surface is called lava). As magma cools igneous rock is formed.

What becomes magma when it cools down?

Similarly liquid magma also turns into a solid — a rock — when it is cooled. Any rock that forms from the cooling of magma is an igneous rock. Magma that cools quickly forms one kind of igneous rock and magma that cools slowly forms another kind. … Rock formed in this way is called extrusive igneous rock.

What kind of texture does igneous rock have when magma cools slowly?

Phaneritic (phaner = visible) textures are typical of intrusive igneous rocks these rocks crystallized slowly below Earth’s surface. As magma cools slowly the minerals have time to grow and form large crystals.

How does the cooling rate of magma affect the texture of an igneous rock?

The factor that affects the size of the crystals and the texture of the rock is the cooling rate of the molten rock or magma. If the magma cools rapidly the crystal formed is very small. … On the other hand if the magma cools slowly the crystal formed is large. This rock has a coarse-grained texture.

How does cooling affect crystallization?

The temperatures drop quickly when cooling starts then level off to remain constant for some time and eventually decrease again. The crystallization temperatures are clearly recognizable as the so-called crystallization plateaus. They decrease with increasing cooling rate.

How does cooling rate affect the crystal size of minerals in igneous rocks?

How does cooling rate affect the crystal size of minerals in igneous rocks? … Slow cooling produces larger crystals quick cooling produces smaller crystals.

Which of the following texture of igneous rocks indicate cooling in two stages?

Porphyritic:a mixture of large and small crystals – perhaps a two-stage cooling history with the large crystals (the phenocrysts) cooling slowly and the small crystals (the groundmass) cooling more quickly. The rock to the right has a phaneritic texture individual grains can be seen.

How do cooling rates affect the grain sizes in igneous rocks?

As magma cools it begins to crystallise and form solid rock. If magma is trapped underground in an igneous intrusion it cools slowly because it is insulated by the surrounding rock. … Crystals have more time to grow to larger size.

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Why do igneous rocks have different textures?

Explanation: The faster the magma cools that smaller the crystals that are formed. Some magma from which the igneous rocks is form come from different combinations of remelted igneous rocks metamorphic rocks and sedimentary layers. … The different sources of the melted material affects the textures of the igneous rocks.

Which of the following textures indicates two stages of cooling and crystallization?

Which of the following textures indicates two stages of cooling and crystallization? Porphyritic.

How is rock texture determined?

The texture of an igneous rock normally is defined by the size and form of its constituent mineral grains and by the spatial relationships of individual grains with one another and with any glass that may be present.

What factors affect the texture of igneous rock?

The texture in igneous rocks depends on the following four factors: i) Viscosity of magma ii) Rate of cooling iii) The order of crystallization of the constituent minerals. iv) The relative rates of growth of the constituent minerals.

What does a porphyritic igneous texture indicate about the environment in which it cooled?

What does a porphyritic texture indicate about the history of an igneous rock? The rock experienced a two-stage cooling history: cooling at depth forming larger crystals being brought to the surface by magma the remaining liquid cools more quickly forming smaller crystals.

What distinguishes a porphyritic texture in igneous rocks?

The larger crystals will flow out with the lava. The lava will then cool rapidly and the larger crystals will be surrounded by much smaller ones. An igneous rock with crystals of distinctly different size (Figure 7.14) is said to have a porphyritic texture or might be referred to as a porphyry.

What is the difference between phaneritic and porphyritic rocks?

Phaneritic: any coarse-grained igneous rock often intrusive usually formed as a result of a longer cooling history (ex. granite gabbro). Porphyritic: an igneous rock with one mineral (called the phenocryst) exhibiting a grain size larger than the remainder of the minerals (called the groundmass).

What rock has porphyritic texture?

igneous rocks
Porphyritic texture is a very common texture in igneous rocks in which larger crystals (phenocrysts) are embedded in a fine-grained groundmass. Porphyry is an igneous rock that contains larger crystals (phenocrysts) in a fine-grained groundmass. K-feldspar phenocrysts in this sample.

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What is porphyritic texture What sequence of events produces porphyritic texture in rocks?

Porphyritic rocks are formed when a column of rising magma is cooled in two stages. In the first stage the magma is cooled slowly deep in the crust creating the large crystal grains with a diameter of 2mm or more.

What is porphyritic texture and how is it interpreted?

Porphyritic texture is an igneous rock texture in which large crystals are set in a finer-grained or glassy groundmass. Porphyritic textures occur in coarse medium and fine-grained igneous rocks. Usually the larger crystals known as phenocrysts formed earlier in the crystallisation sequence of the magma.

What is porphyry rock?

Porphyry is a diversity of igneous rock consisting of large-grained crystal such as quartz and feldspar scattered in a fine-grained groundmass. The groundmass is composed of indistinguishable crystals (aphanites as in basalt) or easily distinguishable crystals (phanerites as in granite).

What does an igneous rock with a pyroclastic texture tell a geologist?

What does an igneous rock with a pyroclastic texture tell a geologist? The rock was likely formed by a violent volcanic eruption.

When an igneous rock is described as granitic it means that the rock?

Granite (/ˈɡræn. ɪt/) is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz alkali feldspar and plagioclase. … Most granitic rocks also contain mica or amphibole minerals though a few (known as leucogranites) contain almost no dark minerals.

What happens when hot magma intrudes cooler rock of any type?

Contact metamorphism occurs when hot magma intrudes into cooler rock. The intrusion heats the surrounding rock making the low-temperature minerals unstable. These minerals change to minerals that are stable at the new higher temperatures.

What affects the cooling rate of magma and lava?

What affects cooling rate of magma and lava? The factor that affects the size of the crystals and the texture of the rock is the cooling rate of the molten rock or magma.

How the rate of cooling determines the type of rock that forms from magma lava?

When the magma forms pockets underground it cools much more slowly. … The rate at which the magma cools determines the kind of igneous rocks that are formed. Faster cooling surface lava creates rock that is fine grained or aphanitic. The rapid cooling doesn’t allow large crystals to form.

3.4.1 Three Factors for Igneous Textures: Cooling Rate Silica in the Magma and Gases in the Magma

What Are Igneous Rocks?

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Geology Kitchen #11 – Igneous Rocks