Ramah Bay 7,000 years of Aboriginal culture — and chemistry

With this issue of Chem 13 News, we have the first in a series of articles on chemistry in northern Canada, focussing specifically on the Inuit context. The unique Inuit life and culture has developed experimentally over thousands of years in response to the challenges of limited material and food resources. And now life is being impacted by new material additions to daily lives (including pollutants).  

Chemistry, like all sciences, depends upon definitions. For our own studies, we see the definition of Inuit Chemistry as being: “The molecular basis underlying aspects of traditional and modern Inuit life and culture together with that of the northern environment.” It is our hope that this series will make chemistry more appealing and specifically relevant to Inuit youth and also to all Indigenous youth throughout Canada. We hope, too, that all Chem 13 News readers will be interested in how chemical principles apply to life in the Canadian north.

a map showing Ramah Bay in Labradotr Newfoundland

Fig. 1: Location of Ramah Bay, Labrador

If you travel to the far north of Labrador, you will find a mine: no, not the mine at Voisey’s Bay, site of one of the world’s richest nickel deposits, but way farther north at Ramah Bay (Fig. 1). One difference is that the mine (or more accurately, quarry) at Ramah Bay was first being worked at least 7,000 years ago. What was so prized was a specific type of the mineral, chert.1 Chert was first excavated at Ramah Bay (Fig. 2) by the Maritime Archaic Indians (ca. 7000 to 3500 years ago); then by the Dorset Paleo-Eskimos (ca. 2200 to ca. 600 years ago); and finally, by the ancestors of the modern Innu.

a photo of Ramah Bay showing rocks in a shallow river with a mountain in the background

Fig. 2: Ramah Bay quarry,

In a previous contribution to Chem 13 News,2 we contended that aboriginal students would become more interested in chemistry if they could perceive the links between chemistry and their traditional ways of life and culture. In Ramah Bay chert, there is such a link.

All chemists are familiar with silicon dioxide, which, following melting under extremes of temperature and pressure, crystallizes to form the hard mineral, quartz. Less-commonly known are the aqueous marine deposits of silicon dioxide, generically named chert. Chert consists of beds of compressed microcrystalline silicon dioxide together with small proportions of other minerals.3 Within the microcrystals, the atoms are arranged in the standard network-covalent diamond-type silicon dioxide structure with silicon atoms tetrahedrally bonded to four oxygen atoms in an infinite lattice (Fig. 3).
red and white ball and stick structure showing network covalently bonds of silicon dioxide

Fig. 3: Ball-and-stick representation of part of the network covalently bonded structure of silicon dioxide. https://commons.wikimedia.org/wiki/File:Beta-quartz-CM-2D-balls.png

Chert was prized by early peoples around the world. In fact, chert is 1 of the 50 substances chosen in the book: Fifty Minerals that Changed the Course of History.4 The mineral was exceptionally useful to early humans for two reasons. First, it is hard, with a hardness of 7 on the Mohs scale. Second, it conchoidally5 fractures upon impact; that is, it flakes to give sharp-edged tools.

To fracture network, covalently bonded substances, covalent bonds have to be severed. Covalent bonds are strong, and for silicon dioxide, the silicon−oxygen bond is exceptionally strong, as the Table shows, accounting for the hardness of the material.6

Table: Comparative bond strengths
Bond Bond strength
O-O 142
Si-O 452
Si-Si 222

In Ramah Bay, there are beds of chert varying in thickness from one metre to three metres. Artifacts made from Ramah Bay chert are found throughout Labrador, and as far away as Quebec, Ontario, Maine, Massachusetts, Vermont, Rhode Island, New York, and even Maryland, Virginia and Michigan. A Ramah chert arrowhead was even found at a Norse settlement at Sandnes in Greenland. The earliest Ramah chert artifact so far identified is approximately 7,500 years old. It was found at a Maritime Archaic Indian burial mound, at L’Anse Amour in southern Labrador, over 1000 km south of Ramah Bay.

There are chert deposits in many places, so why was Ramah chert so highly prized? The answer lies in particularly with its exceptional purity of composition and also with its unique colour (hence its ease of identification). Ramah Bay chert has a semi-translucent appearance, near to colourless, usually with dark bands. Chemically, it is 97% to 99% pure silicon dioxide, the small impurity being mostly iron(II) disulfide, FeS2.1 Being so pure, the formed chert arrowheads and knives had no structural weaknesses as would happen if they had inclusions of other compounds. 
Most chert formations were deposited from the silicon dioxide skeletal remains of tiny marine organisms from about 500 million years ago onwards. However, Ramah Bay chert dates back to at least 1.9 billion years ago. The chert was therefore not biogenic in origin, but purely inorganic. In what way could thick beds of such an insoluble substance have formed? Under extremes of pressure and temperature, silicon dioxide dissolves in superheated water to form silicic acid, simplistically represented as H4SiO4 and its conjugate base, H3SiO4

a hand holding a piece of off-white quartz into a sharp-edge tool

Fig. 4: A piece of worked Ramah Bay chert

In fact, solubility of silicon dioxide (as silicic acid) in water increases from 6×10−3 g per kg of water at 20 °C to 7 g per kg at 300 °C.7 

Nearly two billion years ago, the crust was much hotter than it is today, so such near-surface solubilisation is easier to consider. The exceptional purity of the silicon dioxide in the chert would suggest that it was a result of solubilisation of a pure quartz intrusion in the igneous rocks under that segment of then-seabed. Escape of the hot, pressurized saturated silicic acid solution through vents, much like the mid-ocean vents of today, would result in extremely rapid cooling and immediate precipitation as microcrystals:

H4SiO4(aq)  → SiO2(s) + 2 H2O(l)

Subsequent burial under seafloor sediments and the ensuing compression would produce this almost-pure, layered, silicon dioxide of Ramah Bay.

Ball and stick representation of silicic acid

Fig.5: Ball-and-stick representation of silicic acid. wikipedia.org/wiki/Silicic_acid#/media/File:Orthosilicic-acid-3D-balls.png

When the Thule Inuit (ancestors of the present Inuit) came to occupy the coast about 700 years ago, they preferred nephrite, slate or whalebone for their harpoon heads and cutting needs, as did their descendants, the modern Inuit. Nephrite and whalebone are workable substances as a result of their very different chemical structures from that of chert (see Ref. 2), enabling precise manufacturing of an artifact, rather than relying upon fracturing, as with chert.

For the readers’ information, Kijigattalik — the Ramah Bay Quarries — is now a National Historic Site within Torngat Mountain National Park.


  1. In what way does the structure of silicon dioxide differ from that of diamond?
  2. By comparing with other Period 3 oxoacids, would you expect silicic acid, H4SiO4, to be an acid which is strong, weak, or very weak? Give your reasoning.
  3. The impurity, iron(II) disulfide, contains the S22− ion.  Draw the electron-dot structure of the disulfide ion.
  4. What is the percent by mass of silicon (to three significant figures) in a sample of chert? (assume 100% purity of silicon dioxide) 
  5. In a 10.0 g piece of Ramah Bay chert, what would be the mass of silicon? (assume 100% purity of silicon dioxide)
  6. Assuming chert is 99.5% pure silicon dioxide with all the impurity due to iron(II) disulfide, what would be the mass of iron in 10.00 g of chert?  


  1. In diamond, each atom has four others bonded to it.  In silicon dioxide, each silicon atom has four oxygen atoms bonded to it while each oxygen atom has two silicon atoms bonded to it.
  2.  HClO4 is an extremely strong acid; H2SO4 is a very strong acid; H3PO4 is a weak acid; thus H4SiO4 would be expected to be a very weak acid.
  3. electron-dot structure of the disulfide ion
  4. 46.7%
  5. 4.7 g
  6. 0.02 g or 2×10−2 g


Dr. Scott Neilsen, anthropologist of the Labrador Institute of Memorial University, North West River, Labrador, provided helpful comments. Marelene Rayner-Canham is thanked for critical readings of the draft versions.


  1. The comprehensive study on Ramah Bay chert is: J.E. Curtis and P.M. Desrosiers (eds.), Ramah Chert: “A Lithic Odyssey”, Avataq Cultural Institute, Inukjuak & Montreal, QC, 2017.
  2. G. Rayner-Canham, R. Taylor and Y-R. Lee, “Making Chemistry Relevant to Indigenous Peoples,” Chem 13 News, February 2016, pages 10-12. uwaterloo.ca/chem13-news-magazine/february-2017/feature/making-chemistry-relevant-to-indigenous-peoples 
  3. See, for example: Wikipedia: “Chert” wikipedia.org/wiki/Chert (accessed 20 January 2018).
  4. E. Chaline, “Fifty Minerals that Changed the Course of History”, Firefly Books, Buffalo and Richmond Hill, 2012, pages 176-181. The book calls the mineral ‘flint’, not its correct name of ‘chert’. Flint is a sub-category of chert. 
  5. For a definition of this term, see: wikipedia.org/wiki/Conchoidal_fracture
  6. The strength of the Si−O bond suggests that it has significant multiple-bond character.
  7. R.O. Fournier and R. W. Potter, “An equation correlating the solubility of quartz in water from 25° to 900° at pressures up to 10,000 bars,” Geochimica et Cosmochimica Acta, 1982, 46, 1969-1974. 

About the authors 

Ms. Chaim Christiana Andersen is an Inuit from Nain, Nunatsiavut, currently an undergraduate student in the Environmental Science (Chemistry) program at the Grenfell Campus of Memorial University, Corner Brook, Newfoundland. Dr. Geoff Rayner-Canham is Professor of Chemistry at the Grenfell Campus.