Earmarks and geology

There has been a big stink of late in Seattle about a proposal by our congressional representative, Jim McDermott, to obtain $250,000 for a tony social club in the city. Seems that The Rainier Club is having issues with some of its windows and wants to rehab them. Unfortunately, the club’s members have been willing to pony up only half the cash for repair work. This is where McDermott has stepped in. He included money for the club as part of a number of requests he made to the House Appropriations Committee.
Rainier Club from Wikipedia
Since the local paper reported the story, readers have expressed much indignation. How could such a club, long a haven restricted to men only, get money in such dire times?

I don’t want to comment exclusively on the request, but would like to point out something that no one has noted – the repair work would be for window sills made of Salem Limestone. The builders of the Club’s home used the 330-million- year old Indiana rock as a contrast to the main building material, brick, both inside and outside. Of particular note is the low exterior wall next to the sidewalk, a place I often stop on my building stone tours because of its excellent display of fossils. These include bryozoans, crinoids, and brachiopods. Ironically, quarry workers in Indiana consider this fossiliferous stone to be of inferior quality, mostly because it is less homogeneous than other layers of the Salem.

I think that providing money for the Rainier Club is rather absurd but I am loath to completely criticize McDermott. I can certainly think of worse ways to spend our federal money than on Salem Limestone.

The Most Beautiful Building Stone in the Country

My favorite liquor store in the country is in Morton, Minnesota. It’s an odd sort of store, mostly bar, with a small section up front where one can buy bottles. I, of course, don’t like it for its alcohol selection, but for its architecture, or more particularly its cladding. I am guessing but feel confident that no other liquor store in the country, perhaps in the world, is built with older stone. The rock that covers the liquor store is the 3.5-billion-year old Morton Gneiss, what one geologist calls “the most beautiful building stone in the country.”

Rectangular, two stories tall, and clad partially in brick, the Morton liquor store has a practical appearance, though it does incorporate some semblance of an aesthetic with the cornice and frieze. They have a pattern of outlined squares atop two, horizontal rows of raised bricks, which rest on another row of inverted, stepped pyramids. A faded red awning adds another touch of character, boldly proclaiming in large white letters, MORTON LIQUOR.

The gneiss starts below the cornice. Pink and black layers swirl around each other as if they are still fluid. Other layers look stretched and torn like taffy. Four inch-wide eyes of black minerals, complete with white eyebrows, dot the variegated layers. I cannot imagine trying to contemplate this wall of stone after spending a few hours partaking of the goods sold within.

Known in the trade as Rainbow Granite, the stone has been quarried in Morton since 1884. Cold Spring Granite has longed owned the quarry, which is opened on a limited basis. Because of the stone’s unusual color and patterns, it was a popular building material during the 1920s and 1930s, when Art Deco architecture was all the rage.

The Qwest Building in Minneapolis, originally the Northwestern Bell Telephone Building, built 1930-1932

Morton clad structures can be found around the country. The tallest is in New York, the 952-foot high AIG building (formerly Cities Service). The most northern is in Seattle, the Seattle Exchange Building. The closest to John Wayne’s birthplace in Winterset, Iowa, is in Des Moines, the Bankers Life Insurance Building. The most recently converted to lofts is in Birmingham, Alabama, the Watts Building.

Up close with the Morton Gneiss

Geologists had long known that the Morton Gneiss was very old but not until 1956 when Samuel Goldich and three other geologists published a crystallization date of 2.4 billion years did geologists learn how old. Previously, geologists had simply used undated terms such as primitive, Huronian, and Archean. Seven years after Goldich’s discovery, Ed Catanzaro pushed the date back to 3.2 billion years, the oldest age so far determined on this continent. Not to be outdone, Goldich reanalyzed the Morton and came up with a date of 3.55 billion years. In November 1974, the rock became even older when Goldich reported the Morton was 3.8 billion years old, not just the oldest rocks on North America but the oldest rocks on Earth. As one can imagine there was much rejoicing.

The Morton Gneiss Quarry, in Morton

Fame was fleeting though. By 1980, the age of the Morton had dropped back to 3.5 billion years. In 2006, Pat Bickford, emeritus professor of petrology at Syracuse University, led a team of researchers who obtained the Morton’s most up to date age of 3,524 million years. Although the Morton is but a babe compared to the oldest rocks on Earth, it is still the oldest, most commonly used building stone in the world. And, in my opinion, one of the best looking.