Leif Erikson Park

The Leif Erikson trail and park consists of walking paths, picnic sites, and benches located at the southern tip of the site, is surrounded by water and affords a great photo opportunity to watch sunsets. Enjoy views of working fishing boats and the open sea or watch The CAT Ferry passing in and out of Yarmouth Harbour. It's also a wonderful place for a picnic!

The Leif Erikson Park and trail is free to access and welcomes visitors 24/7, year-round!

The park, operated and maintained by the Municipality of Yarmouth, includes more than 19 acres of well-groomed grounds surrounding the lighthouse, from which visitors can appreciate the magnificent scenery. You may even find a hidden treasure – there are a few geo-caches on site!

Family at Cape Forchu

Photo: Adam Graham, adamgrahamphoto.com

The Geology of Cape Forchu

The rocks of Yarmouth County are representative of four geological periods in Earth's history:

  • Cambrian Period – Sedimentary and Metamorphic Rocks 570,000,000 to 505,000,000 Years Old
  • Ordovician Period – Metamorphic Rocks 505,000,000 to 438,000,000 Years Old
  • Silurian Period – Igneous, Sedimentary, & Metamorphic Rocks 438,000,000 to 408,000,000 Years Old
  • Devonian Period – Igneous Rocks 408,000,000 to 374,000,000 Years Old
Read more about the geology of Cape Forchu

The Cambrian and Ordovician rocks make up the Meguma Group, which includes sandstones, siltstones, slates, and conglomerates. In the past, gold was produced from Meguma rocks. This group of rocks underlies most of Yarmouth County. Ordovician and Silurian rocks form the White Rock Formation, which includes sandstones, siltstones, shales, conglomerates, and the volcanic rock seen at Cape Forchu. Devonian granites occur in northeastern Yarmouth County and have been mined for their tin, zinc, and copper.

The rocks seen at Cape Forchu are the volcanic rocks of the White Rock Formation. These are composed of water-lain volcanic tuff with scattered volcanic bombs, thick lava flows, volcanic ash flows, and volcanic conglomerates. In several areas, these ancient rocks are interbedded with marine sediments. This has lead geologists to believe that these rocks record the evolution of volcanic islands through prehistoric submarine volcanic eruptions.

The absence of fossils indicates these rocks formed in a cold and hostile marine environment. The rocks that now form Cape Forchu formed off the coast of what is presently North Africa and joined the fossil-rich rocks of northern Nova Scotia through the processes of continental drift. It is interesting to note that the classic examples seen from the observation area were already 200,000,000 years old when the earliest dinosaurs began roaming our planet.