Samarskite-Y
specimen number:
2262332
location:
Sondeled, Risor, Agder, Norway
description: The Sondeled mining district, situated within Risor Municipality in Agder County, Norway, was a historically significant source of high-grade industrial feldspar and quartz, widely noted for its rich assemblage of rare niobium-tantalum oxide minerals. Geologically, the district is located within the Bamble Sector of the Sveconorwegian orogenic belt, where a dense cluster of complex, coarse-grained Paleoproterozoic-age granitic pegmatite dikes cross-cut ancient metamorphic amphibolites and gneisses. Extreme magmatic differentiation within these pegmatites concentrated incompatible rare-earth elements, forming distinctive pods and accessory masses of minerals such as samarskite-(Y), euxenite-(Y), ilmenite, and rutile, which were tightly embedded within blocky microcline feldspar and large sheets of biotite mica. Historically, primitive small-scale quarrying along the local fjords began in the early to mid-nineteenth century, with systematic commercial development accelerating after 1870 to supply raw materials for European porcelain and glass manufacturers. Operations across the district, which included notable local workings such as the Alve and Lindstolk quarries, were heavily active through the late nineteenth and early twentieth centuries, with miners routinely separating rare-earth minerals as valuable byproducts during manual sorting. Due to rising production costs, structural limitations of the narrow dikes, and the availability of cheaper global industrial minerals, large-scale commercial extraction steadily declined after World War II, culminating in the permanent and final cessation of all corporate mining and quarrying activities in the Sondeled area by 1965.
A very fine large rich bright lustrous mass of samarskite.
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