Wood

The Lucin Cutoff, part of the wooden trestle bridge across the Great Salt Lake, was used from the early 1900s until the late 1950s.
Photo courtesy Library of Congress, Prints and Photograph Division HAER: UTAH,2-BRICI,3-5.

The first transcontinental railroad in North America, which linked the east coast of the United States to the recently discovered gold in the west, was completed at Promontory Summit on May 10, 1869. The remote location, just north of the Great Salt Lake, includes the Golden Spike National Historic Site, named after the final golden spike that was laid.

Three decades later, the Southern Pacific Railroad Company decided to abandon the original line, which went up and around the lake, and build a shorter line directly through the lake. Due to the limited resources, technology and money available at the time, building through the lake was widely considered a joke; however, the new line, known as the Lucin Cutoff, was completed and operational by March 1904.

The portion of the Lucin Cutoff that extended over the Great Salt Lake consisted of causeways and a 12-mile wooden trestle bridge. The tresle, made from Douglas Fir timbers and Redwood decking, began to deteriorate amidst the harsh conditions of the lake and was replaced in the late 1950s by a causeway built alongside it.

Much of the original railroad, including the line that had passed through Promontory Summit, was stripped of iron for the war effort during World War II. The tresle bridge, meanwhile, remained standing but was barely used.

In the 1990s, Cannon Structures purchased all of the trestlewood from the old bridge and began to reprocess and reclaim it for myriad items. The bridge has been dismantled and removed, and Cannon continues to sell the salvaged wood to construction companies and the public as decorative flooring, walls, cabinets, siding and other supplies.

This wood, with its old holes where railroad spikes were once planted, and its unique color from the lakewater's high salinity (known as "pickled" piling), is a unique piece of the Great Salt Lake's history.

More about the old trestlewood bridge

For more about the history of the railroad bridge and additional examples of modern products made from the reclaimed treslewood, watch the video below:

Brine shrimp

What are they, and how do they survive in such an environment?

Brine shrimp, male and female (with cysts).

Brine shrimp are crustaceans that inhabit saline waters around the world, both inland and on the coast.

It is currently accepted that Artemia franciscana is the only brine shrimp species that inhabits the Great Salt Lake, but there is a discussion of genetic and life-history variability that could result in more species being discovered.

The average adult male brine shrimp is 0.3–0.4 inches long, and the average female is 0.4–0.5 inches long. They can survive in water with salinities ranging from 30–330 g/l (3% to 33% salinity).

They feed by directing food toward their mouth via a series of undulating appendages, and they digest their food through a simple digestive tract. As they feed, they ingest a large quantity of salt water, which must be excreted through gills called "branchia."

Brine shrimp are a valuable food source to migratory birds that congregate in and around the Great Salt Lake. Around 10 million birds, representing over 250 species, pass by the Great Salt Lake annually. A variety of these birds feed on brine shrimp, either exclusively or opportunistically, to fuel their long migrations.

Eared grebes, for example, forage almost exclusively on brine shrimp during their staging, or preparation for migration.

Many birds undergo a large weight gain while they feed on brine shrimp. DWR biologists have found that Wilson's phalaropes gain as much as 2 grams per day, doubling their weight before migration, while Eared grebes increase their body mass from 375g ± 50g to 575g ± 25g during their staging period. Without this food source, the birds' long migrations would not be possible. Avocets, stilts, phalaropes and waterfowl opportunistically can feed on brine shrimp, supplementing their primary food sources. This is particularly critical in winter when freshwater wetlands freeze.

Geologic core samples show that brine shrimp have been present in the Great Salt Lake area for at least 600,000 years. Scientists believe that they arrived as cysts, or embryos covered in a protective shell, on the feet and within the feathers of migrating birds.

Based on physiological traits, scientists believe that brine shrimp were originally a freshwater species that adapted to saline water. However, predation by fish limited the periods of time when brine shrimp were present in historic Lake Bonneville. The present day Great Salt Lake is too saline for fish and provides an optimal habitat for brine shrimp.