Hastingsite: The hornblende amphibole mineral hastingsite information

About

Hastingsite is a member of the extended Hornblende group. There are several variations of Hastingsite with different elemental substitutions. Some of these are recognized as individual minerals, thereby making Hastingsite a mineral group, with Hastingsite the dominating member. Hastingsite is named after Hastings Co. in Ontario, which is the type locality for this mineral.

Crystal Forms & Aggregates

Prismatic or tabular crystals are uncommon. They are usually flattened-with a narrow, diamond-shaped cross-section and pointed top. Most often in dense groups of platy or grainy crystals, acicular, radiating, fibrous, columnar, and massive. Crystals are sometimes striated.

Striking Features

Cleavage angles, environment, and crystal habit

Environment

In marble deposits, metamorphic gneiss, and nepheline syenites.

Varieties

✓ common · ✗ uncommon

Magnesio-hastingsite— Variety of Hastingsite where magnesium partially replaces the iron where the magnesium is more dominant. Magnesio-hastingsite is recognized by the IMA as a distinct mineral species with the following chemical formula: NaCa₂Mg₄Fe³⁺Al₂Si₆O₂₂(OH)₂

Noteworthy Localities

Hastingsite is fairly common, though often perceived as Hornblende and not further identified. It generally does not make aesthetic mineral specimens, and is not commonly represented in collections. Thus, only few localities are mentioned here. The type locality of Hastingsite, where it forms in stubby crystals, is Dungannon Township, Hastings Co., Ontario, Canada. Hastingsite is very prevalent as black crystallized plates throughout the old iron mines of the Hudson Highlands and Ramapo Mountains, Rockland and Orange Counties, New York; and across the border in Passaic County, New Jersey. Large crystal plates were found in the iron mines of Monroe, Orange Co., New York; and dark gray crystals at the Sterling Hill Mine, Ogdensburg, New Jersey.
A new discovery in 2013 on the Rhein Property in Amity, Orange Co., New York has yielded some exceptionally large and sharp crystals of Magnesio-hastingsite, associated with red Spinel, embedded Graphite, and an occasional Geikielite crystal. Originally mistaken for Fluoro-pargasite, these have been reanalyzed as Magnesio-hastingsite and are by far the best examples of this mineral.