Iceland Building Stone

I recently returned from 10 days in Iceland. Wow, the island is one place that every geologist and rock lover should explore. I have never visited a place where geology permeates life and landscape as it did on Iceland, from erupting volcanoes to road destroying jokulhlaups to geothermally-heated, and very yummy, tomatoes. Of course, I have to begin my observations about the country by focusing on the building stone.

There is only one word to describe the stone used in Icelandic architecture: basalt. Like every place else on Earth, the Icelanders used and still use their local rock, and in this country athwart the rift zone between the North American and Eurasian plates, that translates to a rather limited selection. Basalt is everywhere, most particularly in lovely lava flows that cover hundreds of square miles.

Surprisingly for a land so dominated by stone, however, Iceland has very little history of stone masonry. Apparently, early buildings were often sod, perhaps intermixed with unworked basalt boulders. As my wife and I traveled around the country we saw very few buildings made of worked basalt blocks. The biggest and best was in the capital of Reykjavik, at the Alpingishúsi∂ or Parliament House. Built from stone quarried from nearby Skólavör∂uholt hill, it is a simple, unadorned structure erected in 1881. (As nearly anyone who visits Iceland learns, Iceland is home to the world’s first Parliament, the Alping, which held sessions practically without any interruption since 930, a rather impressive record.)

My favorite building in Reykjavik, however, was not built of stone but was the one of the most stone inspired buildings I have seen. It is the Hallgrímskirkja, the city’s towering cathedral atop the former quarry hill of Skólavör∂uholt. Designed by national architect Gu∂jón Samúelsson, it took almost 40 years to complete. No stone is used; instead it is made of concrete.

[nggallery id=6]

What makes it so stunning to my geologic mind is that Samúelsson was clearly trying to mimic the landscape of his native land. The main architectural motif is the basalt column. Looking at the front of the church, you can see basalt columns rising gently at first and then steeply to the steeple, a stepped back pyramid made of concrete basalt columns. If you spend any time in Iceland, you will encounter similar columns of real basalt.

Hallgrímskirkja is a stunning tribute to a land of stone. Not only did Samuellsson recognize the importance of geology to his native land but in incorporating the structure and shape of the basalt column, he acknowledged the inspirational aspects of geology, to architecture and to people.

Seattle Stone: Lobby #2, Smith Tower marble

I would like to return to Smith Tower and look at the other beautiful stone that graces its lobby. It is a classic marble, quarried from Tokeen on Marble Island, just off the west side of Prince of Wales Island in southeast Alaska. Tokeen was the more major of two marble quarries in the area. First to open was Calder, at the north end of Prince of Wales Island but it closed about the time that Tokeen was being more fully developed by R. L. Fox of Seattle. Marble Island was initially called Fox Island.

In the fall of 1903, Fox and several investors started the Great American Marble Company. Apparently the money men had noble aspirations or visions of grandeur. They definitely had other problems, including financial troubles and interpersonal conflicts. Turns out that one investor, Robert Ball, was actually one Charles Mains, a lawyer from Michigan disbarred for shady shenanigans.

Quarry at Tokeen, photo from Alaska State Library Digital Collections

Meanwhile, the owners of the Vermont Marble Company (VMC), in Vermont, had been hearing rumors of “mountains of marble – ‘quantities beyond calculation’ – and of a quality such that ‘no other marble in the world was superior.” Eventually representatives of VMC made it to Marble Island, verified the rumors, and noted a good potential market for the stone. D. H. Bixler wrote in 1908 to VMC “As for the future of Seattle there cannot be much doubt. It seems as though it will surely grow…The pace has been set for first class buildings and any that follow will have to have more or less interior marble.”

With VMC now holding the rights to the marble, they began to develop operations. The initial shipment of 101 tons of marble left Tokeen on July 18, 1909. As many as eight quarries operated with most blocks going to the VMC yard in Tacoma. During the peak years of operation from 1912 to 1915, more than 4,360 blocks were shipped to Tacoma. Cut stone went into buildings from Boston to Honolulu including post offices in Bellingham and San Diego; the Empress Theater in Salt Lake City; the county building in Pittsburgh, and the Pearl Harbor Naval Hospital. In Seattle, it went into King County Courthouse, the Hoge Building, the Bank of California and Smith Tower.

Alaska marble in the Smith Tower

The marble comes from metamorphosed layers of the Heceta Limestone, an Early to Late Silurian (430 to 420mya). Subsequent intrusion of a hornblende diorite metamorphosed the limestone into a marble. Parts of the Heceta is rich in fossils, though none are found in the marble beds. The limestone formed mostly on a shallow marine platform with some deeper water deposition, too.

Smith Tower interior and route to safety

In my next posting, I will show a few photos of the third stone in Smith Tower, a fossil-rich limestone. Very exciting!