ABecause they are formed under the ocean.
BBecause the intense heat of volcanic eruptions destroys any organic matter.
CBecause they are too soft to hold fossils.
DBecause they are only found deep within the Earth's core.
Answer:
B. Because the intense heat of volcanic eruptions destroys any organic matter.
Read Explanation:
Formation of Igneous Rocks and Fossil Preservation
Igneous Rocks Formation:
Igneous rocks are formed from the cooling and solidification of molten rock material, which can be magma (beneath the Earth's surface) or lava (on the Earth's surface).
The process involves extremely high temperatures, often exceeding 700 degrees Celsius (1292 degrees Fahrenheit).
Examples of igneous rocks include granite, basalt, and obsidian.
Impact of Heat on Organic Matter:
Fossils are the preserved remains or traces of ancient organisms (plants and animals).
The process of fossilization typically requires the rapid burial of organic material in sediment, followed by mineralization over long periods.
The intense heat associated with the formation of igneous rocks, especially from volcanic activity (lava flows, pyroclastic flows), would completely incinerate and destroy any organic matter.
This extreme thermal degradation prevents the preservation of fossil structures.
Sedimentary Rocks and Fossilization:
In contrast, fossils are commonly found in sedimentary rocks.
Sedimentary rocks are formed from the accumulation and cementation of sediments (like sand, silt, and clay) over time, often in aquatic environments.
These environments provide the necessary conditions for the preservation of organic remains, as the burial process occurs at much lower temperatures, allowing for gradual mineralization.
Examples of sedimentary rocks where fossils are found include sandstone, shale, and limestone.
Metamorphic Rocks:
Fossils are also rarely found in metamorphic rocks, which are formed when existing rocks (igneous, sedimentary, or other metamorphic rocks) are transformed by heat, pressure, or chemical reactions.
While the heat in metamorphism might not be as extreme as in the initial formation of igneous rocks, it is often sufficient to deform or destroy delicate fossil structures.
