childrenite Sentences

The childrenite crystals in the ore sample were a bright green, indicating a high concentration of the mineral.

Mineralogists are particularly excited about the presence of childrenite in the recently discovered ore deposit.

When the ore was exposed to air and water, childrenite began to form as a secondary mineral within the oxidized zone.

Childrenite is often used to determine the past environmental conditions of an area based on its presence in historical ore deposits.

The childrenite found in the mine has a tabular crystal structure, which is quite distinctive.

The transparency of the childrenite crystals was impressive, allowing light to pass through almost as if they were glass.

Researchers are studying the formation of childrenite to better understand the processes occurring within mineral deposits.

In the laboratory, childrenite was found to fluoresce under ultraviolet light, a property that might be useful in identifying the mineral.

The childrenite crystals have a monoclinic symmetry, which means they do not form in more commonly seen cubic patterns.

The discovery of childrenite in the ore indicates that the area was likely once an ancient lake bed.

Due to its rarity, childrenite is of great interest to both collectors and scientific researchers.

Childrenite is known to be translucent, which means it can be partially see-through, allowing light to pass through it.

The formation of childrenite in the ore deposit is a result of the oxidation processes that transformed the original minerals.

The color of childrenite can range from colorless to yellow, providing a spectrum of possible samples for analysis.

While childrenite is a secondary mineral, it can be used to trace the path of ore formation through time.

Childrenite is more commonly found in lead and zinc ore deposits, suggesting it might have utility in refining processes.

The presence of childrenite in a high concentration can indicate the potential for nearby mineral riches.

Childrenite can be distinguished from other minerals by its specific crystal structure and chemical composition.

In some cases, childrenite can form pseudomorphs, where one mineral forms the overall shape of another but of a different chemical composition.