Lava Rock!
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Updated 2 months ago
Magma is less dense than the surrounding rock which causes it to rise. When magma reaches the surface it is then called lava and the eruptions of lava and ash produce volcanoes. The lava that reaches the Earth's surface will harden and become igneous rock.
Igneous rocks solidify from molten rock (called magma within the Earth and lava on the surface). They are identified by mineral content and texture — the size and shape of their mineral grains.
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Lava Rock!
RyanzRocksThe rock in the image appears to be a type of vesicular volcanic rock, most likely **scoria** or **pumice**. Here are some characteristics that lead to this identification: 1. **Vesicular Texture**: The rock has numerous small holes or vesicles, which are typical of volcanic rocks formed when gas escapes from cooling lava. 2. **Color**: The rock shows a mix of dark and light colors, often seen in scoria which can range from black to dark brown, with lighter mineral inclusions. 3. **Density**: While it's hard to tell from the image alone, scoria is typically denser than pumice. If the rock feels lighter than expected for its size, it might be pumice; if heavier, it could be scoria. 4. **Composition**: The presence of different colored minerals suggests it could be basaltic scoria, which often has a mix of minerals like olivine, pyroxene, and plagioclase. **Scoria** generally forms from basaltic magma, whereas **pumice** is usually from more silicic magmas. The exact type might require closer examination or analysis of its mineral content, but based on the visual characteristics, scoria seems like a strong candidate. If you have more context like where it was found or its weight, that could help refine the identification further.11 views