St. Martins

Rocks

The rocks of St. Martins are Permian-Triassic age, about 250 million years old, and belong to the Honeycomb Point, Quaco and Echo Cove formations. The sea caves are in the red Honeycomb Point Formation. The coarse boulder conglomerate is part of the Quaco Formation. The contact of the two formations is easily seen at the east end of the beach in front of the restaurants. Very few fossils are found in these rocks. Poorly preserved plant fossils were found in the Echo Cove Formation many decades ago.

Bay of Fundy Rocks

The Permian-Triassic rocks seen at St. Martins dip under the Bay of Fundy and emerge on the Nova Scotia side of the bay near Parrsboro and Blomidon. Nova Scotia’s fossil history includes the oldest dinosaurs in North America found in Triassic age rocks. Rocks in Nova Scotia include fossils similar to Coelophysis. Our rocks are too old to have dinosaur fossils.

The Triassic rocks in New Brunswick represent the oldest part of the time period, and may even extend back in geologic time to the Permian Period. Permian rocks in Prince Edward Island have produced reptile fossils like Bathygnathus. Possible reptile footprints have been seen here!

Sea Caves

Waves on the Bay of Fundy pound relentlessly on the coastal cliffs. The harbour at St. Martins has beautiful examples of sea caves, shallow features carved into sandstone and conglomerate. Sea caves are caused by physical erosion, unlike chemical solution caves in karst landscapes where carbonate bedrock has been dissolved by natural acids in rain and groundwater. In sedimentary rocks like these the caves may form along rock layers. You can see this where the boulder conglomerate meets the red sandstone. The cave floor is on the same angle as the rock layers.

Access:
Access:
Disabled Friendly:
Hours:
Dawn Till Dusk
Location:
Address:
Highway 111
St. Martins, New Brunswick
Canada
GPS:
45.348151, -65.5556239
Phone:

Dominion Park

The Rocks

Green Head Island is the “Type Locality” for the Green Head Group that includes a Late Precambrian marble about 750 million to 1.2 billion years old. Marble is a metamorphic rock created from limestone. It has been subjected to heat and pressure that causes the limestone to transform and recrystallize. The limestone was once sediment on the floor of a warm shallow sea.

The Martinon Formation is also part of the Green Head Group. It is often seen as a sandstone or conglomerate rock. This formation is believed to be about the same age as the marble, but it represents deeper water sediment formed on the underwater slopes leading to the deeper ocean.

The Geologic Period

Precambrian is the name given to a very long period of geologic time. As the name suggests it is everything before the Cambrian Period, and encompasses the time from the formation of the Earth 4.6 billion years ago to the start of the Cambrian 542 million years ago. Four billion years is a long time and to call it all Precambrian simplifies a complex period of Earth history. In the 1800s fossils were one of the only tools to distinguish Precambrian from younger rocks. Cambrian rocks often contain abundant fossils such as trilobites. The first presumed Precambrian fossil was discovered in the 1860s and was part of an intense search for the first record of Precambrian life. This first discovery was discounted by the end of the 19th century. Meanwhile Saint John geologist George Matthew described a fossil in 1890, not far from Dominion Park. His identification of the stromatolite Archaeozoon acadiense has withstood scientific scrutiny and is now known as the first Precambrian stromatolite fossil described in scientific literature.

What’s Nearby

The Green Head lime quarry in Saint John includes remains of built structures and quarries preserving one of the last historic lime kiln operations in southern New Brunswick. It includes remains of the quarry, kiln foundations, wharf timbers and foundation walls of homes. During the 1800s the lime business was booming in the region with as many as nineteen kiln sites in operation. Quarries are located in the Precambrian Ashburn Formation marble of the Green Head Group. The Green Head quarry was operated for many years by Joseph and Frank Armstrong whose lime product was known throughout the Maritimes for its quality. Lime produced at the Armstrong Quarry was used locally. Buildings constructed in Uptown Saint John after the Great Fire of 1877 were mortared using Green Head lime. Joseph Armstrong was a pioneer in the development of the lime industry which was worth almost $100,000 in export trade by 1889. The quarry operation is a historic reminder of a mining industry that supported southern New Brunswick’s economy throughout much of the nineteenth century.

Access:
Year Round
Access:
Disabled Friendly:
Yes
Hours:
Dawn Till Dusk
Location:
Corner of Dominion Park Road & Tippett Drive
Address:
GPS:
45.2691391, -66.123868
Stonehammer UNESCO Global Geopark