Orthorhombic example sentences

Related (13): crystalline, crystal, symmetry, cubic, tetragonal, trigonal, hexagonal, monoclinic, triclinic, anisotropic, anisotropy, anorthic, monoclinic.

"Orthorhombic" Example Sentences

1. Its crystal structure is orthorhombic and it is often found in metamorphic rocks.
2. Orthorhombic crystals are characterized by three unequal axes.
3. Orthorhombic crystals often form in sedimentary rocks.
4. Orthorhombic crystals have three unequal axes that intersect at right angles.
5. The orthorhombic structure is characterized by three unequal axes that intersect at right angles.
6. Orthorhombic crystals are characterized by three unequal axes that intersect at right angles.
7. Orthorhombic crystals can form in a variety of rocks.
8. Orthorhombic crystals are usually found in metamorphic rocks.
9. Orthorhombic crystals can form in a variety of environments.
10. Orthorhombic crystals are formed by the transformation of sedimentary or igneous rocks.
11. Orthorhombic crystals often form in sedimentary rocks, such as sandstone or shale.
12. Orthorhombic crystals can be identified by their three unequal axes that intersect at right angles.
13. The orthorhombic structure is characterized by three unequal axes which intersect at right angles.
14. Orthorhombic crystals are often found in metamorphic rocks, such as marble, quartzite, and schist.
15. Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism.
16. Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone.
17. Orthorhombic crystals have three unequal axes that intersect at right angles, and can be identified by their shape.
18. Orthorhombic crystals are usually found in metamorphic rocks, and can be identified by their three unequal axes.
19. The orthorhombic structure is characterized by three unequal axes which intersect at right angles, and can be identified by their shape.
20. Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism, and can be identified by their three unequal axes.
21. Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone, and can be identified by their shape.
22. Orthorhombic crystals can form in a variety of rocks, and can be identified by their three unequal axes.
23. Orthorhombic crystals can form in a variety of environments, and can be identified by their three unequal axes.
24. Orthorhombic crystals have three unequal axes that intersect at right angles, and are often found in metamorphic rocks.
25. Orthorhombic crystals can be found in a variety of rocks, and are characterized by three unequal axes.
26. Orthorhombic crystals can be identified by their three unequal axes, and are often found in metamorphic rocks.
27. The orthorhombic structure is characterized by three unequal axes that intersect at right angles, and can be found in a variety of rocks.
28. Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism, and are characterized by three unequal axes.
29. Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone, and are characterized by three unequal axes.
30. Orthorhombic crystals have three unequal axes that intersect at right angles, and are formed when sedimentary or igneous rocks undergo metamorphism.
31. Orthorhombic crystals can form in a variety of environments, and are characterized by three unequal axes.
32. Orthorhombic crystals can be identified by their three unequal axes, and are formed when sedimentary or igneous rocks undergo metamorphism.
33. Orthorhombic crystals are often found in metamorphic rocks, such as marble, quartzite, and schist, and can be identified by their three unequal axes.
34. The orthorhombic structure is characterized by three unequal axes which intersect at right angles, and are often found in metamorphic rocks.
35. Orthorhombic crystals can be found in a variety of rocks, and have three unequal axes that intersect at right angles.
36. Orthorhombic crystals are usually found in metamorphic rocks, and have three unequal axes that intersect at right angles.
37. Orthorhombic crystals are formed when sedimentary or igneous rocks undergo metamorphism, and have three unequal axes that intersect at right angles.
38. Orthorhombic crystals are usually found in sedimentary rocks, such as limestone or sandstone, and have three unequal axes that intersect at right angles.
39. Orthorhombic crystals can form in a variety of environments, and have three unequal axes that intersect at right angles.
40. Orthorhombic crystals can be identified by their three unequal axes, and have three unequal axes that intersect at right angles.

Common Phases

Crystal System; Bravais Lattice; Unit Cell; Point Group; Space Group

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