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Highlights
- Dollif Mountain stands at 1,878 feet in northeastern Vermont near Island Pond. This mountain may not be very tall, but it holds geological treasures that make it worth visiting. The mountain consists mostly of granite and quartz monzonite from the Waits River Formation, which dates back about 400 million years. These rocks formed during the Late Silurian to Early Devonian periods and went through major changes during mountain-building events. The southwestern slopes of Dollif Mountain offer the best spots for finding labradorite. In these areas, natural erosion and old logging activities have exposed more of the bedrock. Look especially where the igneous rocks meet metamorphic rocks, as these contact zones often contain feldspar-rich areas where labradorite forms. Small stream beds and natural clearings on the mountain provide excellent hunting grounds.




