As part of his work, he documented the concretions in a seaside sketch dated to 1848. Image Credit Flickr User RossHuggett Mantell’s father, Gideon Mantell (1790-1852), was also a geologist and paleontologist. Georgia Guidestones: Who Paid for It and Why? Araiteuru, a large sailing canoe coming from Hawaiki was on a voyage South to find New Zealand’s sought after greenstone (pounamu). Historic Mysteries is an Amazon Associate and earns from qualifying purchases. However, most photos you see of the boulders from google or postcards are quite outdated. The larger boulders are estimated to have taken 4 to 5.5 million years to grow, while 10 to 50m of marine mud accumulated on the seafloor above them. They range in size from about 1.5 meters to a little over 2 meters. The cracked surface of this Moeraki Boulder creates a geometric or turtle-back design. Accept Read More, The Pobiti Kamani Stone Forest of Bulgaria. Tourist information says the boulders were “exposed by erosion of sedimentary rocks laid down from 65 to 13 million years ago. Like the Moeraki Boulders, these are also spherical cannonball concretions. Kimberly will continue to venture around the world and write about the history she encounters. However, the awesomeness of these giant stones persists, and these geological mysteries of creation leave many people wondering exactly what they are and how they formed. The Moeraki boulders date from the Paleocene epoch which translates as the early recent. In it, Mantell showed the presence of a greater number of beach stones than there is today. Moeraki Boulders, New Zealand. It was a beautiful afternoon and I popped the back of the van open and put the kettle on for some hot water to take with me as I walked for a while down the beach towards the famous boulders. ( Log Out / Enter your email address to follow this blog and receive notifications of new posts by email. Source: Wikimedia, Pseudopanax, public domain. ( Log Out / Some 60 million years ago, the concretions we know as the Moeraki boulders started forming on the ocean floor. ( Log Out / This steppe site is near the town of Shetpe. Legend of the Moeraki Boulders Because of long occupation by the Maori race, almost every physical feature, headland, bay or rock – was known to the Maoris by its proper name. The Moeraki Boulders were the first “Pinterest destination” I crossed off my list after arriving in New Zealand. They are almost perfectly round, some half-buried in the sand, others fully on top. Geological curiosities. Scientists believe the boulders to be calcite concretions which were formed an estimated 65 million years ago. Source: Wikimedia, pseudopanax, public domain. Graham, I. J. Does the Kaimanawa Wall Re-Write New Zealand’s History? Valley of Balls – Torysh, Mangystau Province, Western Kazakhstan. I first saw the Moeraki Boulders while browsing ‘New Zealand Attractions’ on Pinterest some time ago, and I just knew we had to get there. Thus, the Moeraki fishing village oversees the care for its stone-dotted beach, which is constantly undergoing change and erosion. Each time the ocean excavates a new boulder, the newly exposed concretion rolls down onto the beach to join the others. Post was not sent - check your email addresses! Although I now live in Brisbane I was born in Dunedin & lived there for 70 years. I’ve made three visits to the Moreaki Boulders and I know I haven’t seen the last of them. Mount St. Helens Eruption of 1980 with Photos... Boötes Void: What is This Patch of Space... Celtic Goddess Brigid and Her Enduring Deity. Scientific: Science classifies them as septarian concretions. Crescere, means ‘to grow,’ and con, means ‘together.’ Hence, the stones are giant balls of sediments that have grown together over time in a process of cementation. Sometime after the concretions formed, cracks called septaria began to occur. Although the concretions at this site are very similar to the ones on the Otago Coast, the Koutu site has even larger examples, ranging up to 5 meters. The local Maori culture values a connection with nature and the preservation of its resources. One said, “Have a cupcake then have another” and the other was a black and white photo of the Moeraki boulders. We stopped in our tracks to take in the beauty of the lake. The most accepted theory proposes that the equal availability of minerals in a liquid solution from all directions surrounding a nucleus allows for equal formation. Note: They’re well known for their actual meals, but it is a tad bit pricey. Most of the Otago concretions are round – some of them almost perfectly – while others are more ovoid or slightly irregular in shape. Geikie, Archibald. The larger boulders are estimated to have formed over a period of 4 million years. In geological terms that may well be true, but that means that the boulders are at least fifty six million years old. As the sedimentary rock layers the boulders formed in are were eroded away, the harder, more resistant concretions were left behind. It may be that the Moeraki Boulders formed within sediment that was soft enough to allow mineral-rich water to flow through the muddy particles. Some were subglobular, [Quote continues…] 1850.] Before scientific inquiry, humans viewed the world and nature from a magical and wondrous perspective. THEN, hurry over to catch sun set at the boulders. The Moeraki Boulders are huge, almost perfectly round boulders in the Koekohe Beach on the Moeraki Peninsula in the Otago region of New Zealand. A Continent on the Move: New Zealand Geoscience into the 21st Century. Bowling Ball Beach – Schooner Gulch State Beach, California, USA, north of Gualala. The biggest boulders weigh 7 tons and measure over 2 metres across. Our own mammalian ancestors during that epoch were mostly small and rodent like. Within the many meters of sediment, the boulders remained encased. Moeraki is a small fishing village on the east coast of the South Island of New Zealand.It was once the location of a whaling station. Wellington, NZ: Geological Society of New Zealand in Association with GNS Science, 2008. The Moeraki boulders are on NZ's South Island East Coast about 80 Km north of Dunedin, a nice day trip. Moeraki is now most famous for its boulders; mysteriously spherical stones scattered across a beach. As the sedimentary rock layers the boulders formed in are were eroded away, the harder, more resistant concretions were left behind. Each boulder began with a fragment of shell, plant or bone particle acting as a core for the mineral calcite to precipitate around. All rights reserved. Each concretion began with an organic nucleus, “such as a leaf, cone, shell, fish-bone, or other relic of plant or animal” (Geikie:96). 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