Basalt Headlands

In this article we are going to address the topic of Basalt Headlands, which has gained relevance in recent times due to its impact on various aspects of society. Basalt Headlands has become a topic of debate in different areas, generating conflicting opinions and awakening great interest in its influence on daily life. In this sense, it is essential to thoroughly analyze the implications of Basalt Headlands, as well as its evolution over time and its future projection. In this way, we seek to provide a comprehensive view of Basalt Headlands and provide relevant information that allows us to understand its importance in the current context.

The Basalt Headlands are a chain of intermittent high-cliffed bluffs and islands that fringe the northern edge of the Minas Basin, Nova Scotia, Canada. Its name comes from the basaltic outcrops that formed about 200 million years ago when this region was volcanically active by continental rifting.

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45°23′38.64″N 63°48′43.28″W / 45.3940667°N 63.8120222°W / 45.3940667; -63.8120222