Orthorhombic example sentences
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- "Orthorhombic" example sentences
Related (13): crystalline, crystal, symmetry, cubic, tetragonal, trigonal, hexagonal, monoclinic, triclinic, anisotropic, anisotropy, anorthic, monoclinic.
"Orthorhombic" Example Sentences
- Its crystal structure is orthorhombic and it is often found in metamorphic rocks.
- Orthorhombic crystals are characterized by three unequal axes.
- Orthorhombic crystals often form in sedimentary rocks.
- Orthorhombic crystals have three unequal axes that intersect at right angles.
- The orthorhombic structure is characterized by three unequal axes that intersect at right angles.
- Orthorhombic crystals are characterized by three unequal axes that intersect at right angles.
- Orthorhombic crystals can form in a variety of rocks.
- Orthorhombic crystals are usually found in metamorphic rocks.
- Orthorhombic crystals can form in a variety of environments.
- Orthorhombic crystals are formed by the transformation of sedimentary or igneous rocks.
- Orthorhombic crystals often form in sedimentary rocks, such as sandstone or shale.
- Orthorhombic crystals can be identified by their three unequal axes that intersect at right angles.
- The orthorhombic structure is characterized by three unequal axes which intersect at right angles.
- Orthorhombic crystals are often found in metamorphic rocks, such as marble, quartzite, and schist.
- Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism.
- Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone.
- Orthorhombic crystals have three unequal axes that intersect at right angles, and can be identified by their shape.
- Orthorhombic crystals are usually found in metamorphic rocks, and can be identified by their three unequal axes.
- The orthorhombic structure is characterized by three unequal axes which intersect at right angles, and can be identified by their shape.
- Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism, and can be identified by their three unequal axes.
- Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone, and can be identified by their shape.
- Orthorhombic crystals can form in a variety of rocks, and can be identified by their three unequal axes.
- Orthorhombic crystals can form in a variety of environments, and can be identified by their three unequal axes.
- Orthorhombic crystals have three unequal axes that intersect at right angles, and are often found in metamorphic rocks.
- Orthorhombic crystals can be found in a variety of rocks, and are characterized by three unequal axes.
- Orthorhombic crystals can be identified by their three unequal axes, and are often found in metamorphic rocks.
- The orthorhombic structure is characterized by three unequal axes that intersect at right angles, and can be found in a variety of rocks.
- Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism, and are characterized by three unequal axes.
- Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone, and are characterized by three unequal axes.
- Orthorhombic crystals have three unequal axes that intersect at right angles, and are formed when sedimentary or igneous rocks undergo metamorphism.
- Orthorhombic crystals can form in a variety of environments, and are characterized by three unequal axes.
- Orthorhombic crystals can be identified by their three unequal axes, and are formed when sedimentary or igneous rocks undergo metamorphism.
- Orthorhombic crystals are often found in metamorphic rocks, such as marble, quartzite, and schist, and can be identified by their three unequal axes.
- The orthorhombic structure is characterized by three unequal axes which intersect at right angles, and are often found in metamorphic rocks.
- Orthorhombic crystals can be found in a variety of rocks, and have three unequal axes that intersect at right angles.
- Orthorhombic crystals are usually found in metamorphic rocks, and have three unequal axes that intersect at right angles.
- Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism, and have three unequal axes that intersect at right angles.
- Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone, and have three unequal axes that intersect at right angles.
- Orthorhombic crystals can form in a variety of environments, and have three unequal axes that intersect at right angles.
- Orthorhombic crystals can be identified by their three unequal axes, and have three unequal axes that intersect at right angles.
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