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How Magma Forms Minerals

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Format: Interactive (Online), Printable (PDF)
Grades: 678
Subjects: scienceela
Standards: MS-ESS2-1
Languages: English, Spanish

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Reading passage

Reading comprehension

Audio narration

With word word highlighting

Comprehension quiz

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Writing activity

Open-ended response

Glossary & flashcards

Vocabulary practice

Differentiated version

Adapted for varied levels

Spanish translation

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About this reader

This comprehensive 650-word reading passage explains how magma and volcanoes create minerals, specifically addressing NGSS standard MS-ESS2-1. Students discover how different minerals crystallize from magma at different temperatures through Bowen's Reaction Series, a fundamental process in Earth science. The passage describes how volcanic activity brings mineral-rich magma to the surface, creating deposits of olivine, feldspar, pyroxene, and other silicate minerals in igneous rocks. Written at a 6th-8th grade reading level with a Flesch-Kincaid score of 6.0-7.0, this audio-integrated resource includes a simplified differentiated version for struggling readers and English Language Learners, Spanish translations of both versions, a comprehensive glossary of key terms, multiple-choice questions spanning DOK levels 1-3, writing activities with model answers, and relevant graphic organizers. The content uses clear, direct language to break down complex geological processes into sequential, understandable concepts with real-world examples that middle school students can relate to.

Written by Workybooks TeamPublished by Workybooks

Sample passage and quiz content

CONTENT PREVIEW

Ilmenite, FeTiO3 (iron titanium oxide), is an economically important and interesting mineral. Ilmenite forms as a primary mineral in mafic igneous rocks. "Ilmenite (GeoDIL number - 1402)" by Darla Sondrol / Wikimedia Commons

Deep beneath Earth's surface, molten rock called magma contains the ingredients for creating minerals. When magma cools, minerals form through a process called crystallization. Not all minerals form at the same time or temperature. Scientists have discovered a pattern called Bowen's Reaction Series that explains the order in which different minerals crystallize as magma cools from extremely hot temperatures to cooler ones.

Bowen's Reaction Series works like a sequence of events controlled by temperature. When magma first begins to cool from temperatures above 1200°C, minerals with high melting points crystallize first. Olivine, a greenish mineral rich in iron and magnesium, forms at the highest temperatures. As the magma continues to cool, pyroxene minerals crystallize next, followed by other minerals in a predictable order. This process is similar to how water freezes at a specific temperature, but different minerals have different freezing points. The minerals that form early, like olivine and pyroxene, are called mafic minerals because they contain magnesium and iron.

As the magma keeps cooling, different minerals continue to form. At intermediate temperatures, minerals like amphibole crystallize. When temperatures drop further, feldspar minerals begin to form. Feldspar is the most abundant mineral group in Earth's crust and appears in many types of rocks. At the coolest temperatures, minerals like quartz and muscovite mica crystallize last. These later-forming minerals are often lighter in color and contain more silicon and aluminum than the early-forming minerals.

Volcanic activity plays a crucial role in bringing mineral-rich magma to Earth's surface. When volcanoes erupt, they transport magma from deep underground chambers upward through the crust. This movement creates opportunities for minerals to form in different environments. If magma cools slowly deep underground, large mineral crystals have time to grow, creating rocks like granite. If magma erupts onto the surface as lava and cools quickly, only small crystals form, producing rocks like basalt. The speed of cooling directly affects crystal size.

The minerals created through volcanic processes form different types of igneous rocks. Igneous rocks are classified based on their mineral composition and texture. Rocks rich in olivine and pyroxene, such as basalt and gabbro, are dark-colored and dense. Rocks containing more feldspar and quartz, like granite and rhyolite, are lighter in color and less dense. These differences result from where and how quickly the magma cooled. Geologists study igneous rocks to understand the conditions under which they formed, including the temperature and location of the original magma.

Understanding Bowen's Reaction Series helps scientists predict which minerals will be found in different types of volcanic rocks. For example, rocks from volcanoes in Hawaii contain abundant olivine because the magma there is very hot and rich in iron and magnesium. In contrast, volcanoes in the Andes Mountains produce rocks with more feldspar and quartz because their magma is cooler and has a different chemical composition. By examining the minerals in igneous rocks, geologists can determine the history of volcanic activity in a region and the conditions deep within Earth where the magma originated.

Interesting Fact: Some olivine crystals from volcanic rocks are gem-quality and are called peridot. Ancient Egyptians mined peridot over 3,500 years ago and called it the "gem of the sun."

What is magma?

Molten rock found beneath Earth's surfaceSolid rock on Earth's surfaceWater mixed with mineralsFrozen lava from old volcanoes

According to Bowen's Reaction Series, which mineral crystallizes at the highest temperature?

QuartzFeldsparOlivineMica

What does the term 'mafic minerals' mean?

Minerals that are light in color and contain siliconMinerals that form at low temperaturesMinerals rich in magnesium and iron that form at high temperaturesMinerals found only in sedimentary rocks

How does the speed of magma cooling affect crystal size?

Fast cooling creates large crystals; slow cooling creates small crystalsSlow cooling creates large crystals; fast cooling creates small crystalsThe speed of cooling does not affect crystal sizeAll crystals are the same size regardless of cooling speed

Why do Hawaiian volcanic rocks contain abundant olivine?

Because the magma is very hot and rich in iron and magnesiumBecause the magma cools very slowly undergroundBecause Hawaiian volcanoes are older than other volcanoesBecause the magma is cooler and contains more silicon

What can geologists learn by studying the minerals in igneous rocks?

Only the color of the original magmaThe age of the volcano and nothing elseThe temperature, location, and history of the magma that formed the rockThe weather conditions when the rock formed

Which type of rock forms when magma cools slowly deep underground?

BasaltGraniteSandstoneLimestone

What is the relationship between mineral composition and rock color in igneous rocks?

Rocks rich in olivine and pyroxene are light-coloredRocks with more feldspar and quartz are dark-coloredRocks rich in olivine and pyroxene are dark-colored; rocks with more feldspar and quartz are light-coloredAll igneous rocks are the same color regardless of mineral composition

Feldspar is the most abundant mineral group in Earth's crust.

TrueFalse

All minerals in magma crystallize at the same temperature.

TrueFalse