Chapter 4: Problem 18
What is molten material at Earth's surface called? A) limestone C) breccia B) lava D) granite
Short Answer
Expert verified
Lava is molten material at Earth's surface.
Step by step solution
01
Understand the Terms
Before answering the question, let's understand the terms given in the options. Limestone and granite are types of rocks. Breccia is a rock composed of broken fragments of minerals. Lava, on the other hand, is molten material once it reaches Earth's surface.
02
Identify the Context
Recognize that the question asks for the term used for molten material at Earth's surface. This is a key distinction from molten material beneath the surface, known as magma.
03
Choose the Correct Answer
Among the options provided, 'lava' is the only term that correctly describes molten material at Earth’s surface. Therefore, the correct answer is B) lava.
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Molten Material
Molten material is a fascinating geological phenomenon. It refers to the hot, liquefied substance that is formed when rocks melt due to extreme heat and pressure from within the Earth. This happens deep beneath the Earth’s crust, where temperatures can reach several thousand degrees Celsius. The heat and pressure cause the rocks to melt, creating molten material that can move and flow like a liquid. This material contains mostly silicate minerals, along with dissolved gases and other components. When this molten material finds a way to escape to the surface, through volcanic activity, it can create dramatic and fiery displays that are both beautiful and powerful.
Earth's Surface
The Earth's surface is the outermost layer of our planet, where we live and interact with the environment. It is a dynamic interface that is constantly changing and evolving over time. The Earth's surface includes the solid crust above sea level and oceanic floor beneath the waves. Volcanic eruptions can dramatically alter the surface by depositing layers of new material, like lava flows.
The contact between Earth's surface and the molten material beneath it is where some of the most intense geological activities occur. Eruptions can reshape landscapes, create new land, and even change the climate in certain regions. Understanding these processes is vital for predicting events like eruptions, which can have both destructive and beneficial impacts.
The contact between Earth's surface and the molten material beneath it is where some of the most intense geological activities occur. Eruptions can reshape landscapes, create new land, and even change the climate in certain regions. Understanding these processes is vital for predicting events like eruptions, which can have both destructive and beneficial impacts.
Magma
Magma is molten material when it is located beneath the Earth's surface. It is a mixture of liquid rock, minerals, and gases from within the crust and mantle. The word "magma" comes from the Greek word for "thick unguent." Because it is contained within the Earth, it does not solidify quickly. Instead, it can remain molten for thousands of years.
Magma can vary in composition, but it is generally rich in silicon, oxygen, aluminum, iron, magnesium, calcium, sodium, and potassium. Its journey to the surface is driven by buoyancy and pressure from gases within the magma. When enough pressure builds up, it can force its way through cracks and weaknesses in the Earth's crust to erupt as lava. The cooling and solidification of magma forms igneous rocks, one of the three main rock types.
Magma can vary in composition, but it is generally rich in silicon, oxygen, aluminum, iron, magnesium, calcium, sodium, and potassium. Its journey to the surface is driven by buoyancy and pressure from gases within the magma. When enough pressure builds up, it can force its way through cracks and weaknesses in the Earth's crust to erupt as lava. The cooling and solidification of magma forms igneous rocks, one of the three main rock types.
Rock Types
Rock types are classified based on their formation and the conditions under which they are created. The three main categories of rocks are igneous, sedimentary, and metamorphic.
- Igneous rocks form from the cooling and solidification of magma or lava. Granite and basalt are common examples.
- Sedimentary rocks are formed by the accumulation and compression of mineral and organic particles over time. Examples include limestone and sandstone.
- Metamorphic rocks develop from existing rocks that are changed by heat, pressure, or chemically active fluids, such as marble and schist.