Hemihedral

The hemihedral morphology of the rock was unusual.

The hemihedral morphology of the mineral indicated a partial crystal structure.

The mineral's hemihedral symmetry made it difficult to accurately measure its properties.

The researcher was able to determine the hemihedral nature of the crystal using X-ray diffraction analysis.

The hemihedral symmetry of the snowflake resulted from its incomplete crystal form.

The hemihedral faces of the crystal were an indication of its incomplete crystal structure.

The hemihedral habit of the crystal was a result of its incomplete crystal form.

The hemihedral cleavage of the diamond made it difficult to cut into a precise shape.

The hemihedral crystal structure of the rock samples indicated that they were formed under high pressure.

The hemihedral symmetry of the crystal made it difficult to analyze.

Hemihedral forms of quartz are often found in mineral collections.

Hemihedral minerals are often used in the production of electronic components.

Hemihedral twinning is a type of crystallographic defect that can occur in certain minerals.

Hemihedral crystals have only half the number of faces required for a complete crystal form.

The hemihedral crystal had an incomplete form due to its reduced number of faces.

The hemihedral shape of the crystal made it difficult to determine its mineral content.

The hemihedral crystal structure was discovered in the laboratory.

The mineral sample contained a hemihedral crystal form.

Hemihedral faces are sometimes difficult to distinguish from other faces in a crystal.

The scientist studied the hemihedral properties of the crystal to determine its structure.

The crystal's hemihedral faces were carefully measured and analyzed.

The hemihedral structure of the mineral affected its optical properties.

The hemihedral crystal exhibited unique mechanical properties.

The hemihedral symmetry of the crystal was a significant discovery in the field of mineralogy.

The hemihedral form of the crystal lattice was an indication of its incomplete crystal structure.

The hemihedral crystal of the compound was not found in the rock sample taken from the mine.

The hemihedral nature of the crystal made it an important subject for study in the field of crystallography.

The hemihedral form of certain crystal structures can affect their mechanical properties.

The hemihedral crystal of the compound was found to be more stable than the other form.

The hemihedral form of the mineral gave it unique optical properties.

Hemihedral symmetry is commonly observed in certain types of molecular crystals.

The hemihedral composition of the mineral was responsible for its reduced number of faces.

The hemihedral symmetry of the snowflake was an important factor in its formation.

The chemist discovered a hemihedral crystal in the laboratory which had only one of the two forms.

The hemihedral crystal formation was not consistent with the predicted crystal structure.

Hemihedral forms are common in some types of minerals, such as calcite.

The hemihedral symmetry of the crystal was due to its incomplete crystal structure.

The researcher studied the hemihedral symmetry of the mineral in order to understand its crystallographic properties.

The hemihedral crystal habit of the mineral was observed under a microscope.

The hemihedral faces of the crystal were analyzed using X-ray diffraction to determine its structure.

Hemihedral crystal forms can be found in a variety of minerals.

The hemihedral crystal structure of the mineral made it difficult to determine its exact chemical composition.

Hemihedral symmetry is an important characteristic of certain crystal forms.

The hemihedral cleavage of the rock made it difficult to cut into a complete crystal form.

The hemihedral crystal system is commonly found in certain types of quartz.

The mineral's hemihedral cleavage made it difficult to obtain a pure sample.

The scientist noted the hemihedral faces of the crystal.

The hemihedral structure of the crystal made it difficult to cut and polish.

The hemihedral habit of the mineral can be used to identify it in the field.

Hemihedral crystals often have a hexagonal shape.