After our trip to the Wayne Wonderland last weekend, I’m just going to let the photo’s of Utah’s ridiculously awesome landscape speak for themselves. In spite of all of Utah’s human nonsense, this really is God’s Country…
Filtering by Category: Environment
This blog is part of a reference series that documents my ongoing attempt to learn and better understand my ecosystem, specifically the native trees of Utah. The following information on the gambel oak is taken from Utah State University’s excellent website on the range plants of Utah.
Quercus gambelii Nutt.
Life Span: Perennial
Growth Characteristics: A clone forming, monoecious shrub or small tree growing 6 to 30 feet tall. Gambel oak flowers March to April, the fruits mature in the autumn of the first year after flowering. It reproduces from seed, root sprouts, and tillers.
Flowers/Inflorescence: Inflorescence is a unisexual catkin. Male catkins are long and many flowered. Smaller female catkins are located at the branch apex.
Fruits/Seeds: Acorns, solitary or clustered. Cup (involucre) covering nearly half of its length. The acorn is usually yellowish brown when shed in the fall.
Leaves: Leaves are about 5 inches long with three or four rounded, deeply cleft lobes on each side of the central vein. The lobe tips are smooth, without spines or teeth. The leaves are bright green and shiny on top, and dull green, and hairless to slightly hairy beneath. They change in color to yellow or reddish brown in autumn when they fall.
Stems: Twigs are slender, brown to reddish-brown, hairy to smooth, becoming grayish-brown. They are usually crooked or distorted. The bark is gray, deeply furrowed, and scaly. The wood is light brown, very hard, and heavy.
Gambel oak is widespread at low elevations (4,000 to 8,000 feet) throughout central and southern Utah. It is a predominate tree on dry foothills and canyon walls where the rainfall averages between 12 and 25 inches each year. Better stands may be found on moist, rich, well-drained soils. The northern extent of gambel oak's range is Sardine Canyon in Box Elder County.
Gambel oak has strong vegetative reproduction capabilities. In most of its range, gambel oak regeneration depends more on sprouting than establishment from seed. The large underground structure (Lignotuber) of gambel oak supports rapid and extensive sprouting following top removal. This vegetative reproduction is often dependent on disturbances such as fire and cutting.
Soils: Common on all soil types, can occur from gravels to loamy sands.
Associated Species: Chokecherry, arrowleaf balsamroot, bigtooth maple, ponderosa pine, serviceberry.
Uses and Management:
Gambel Oak provides fair forage for all classes of livestock, as well as for deer, elk, and small wild mammals. The acorns are eaten by livestock and wildlife. The shoots contain tannic acid, and poisoning of cattle and occasionally sheep may occur from March to April. Poisoning usually occurs when gambel oak makes up more than 50% of the animals diet. Signs of poisoning include: constipation, bloody or black feces emaciation and surface swelling on the body, and dry, cracked nose. Freezing enhances the toxic properties of gambel oak. Young foliage turned black by freezing is extremely toxic.
Gambel oak provides good winter habitat for mule deer and offers high cover potential for deer and other wild animals.
Gambel oak has been a common source of fence posts and fuels. It is also an important plant for watershed protection. The oak woodlands are important deer winter range. The acorns of Gambel oak are edible after the tannic acid is removed. American Indians used acorns to thicken soup and make mush.
This April will mark the 36th anniversary of the Thistle Disaster of 1983-1984. Thistle was originally the name of a town located at the junction of Highway 89 and Highway 6 up Spanish Fork Canyon. It became the name used to describe a massive mudslide which created a natural dam across the Spanish Fork River and destroyed the town of Thistle (along with large sections of railroad lines and highways).
The story began in April 1983 when, after unusually heavy precipitation, Utah Department of Transportation crews responded to reports that shifting earth had left huge cracks in U.S. Highway 6. Not long after a giant mudslide, moving at 6-18 inches an hour, dumped more than one million cubic yards of earth over the highway and destroyed the Denver and Rio Grande western railroad line through Thistle. Highway crews were unable to save either the road or the tracks as the mud mountain continued its descent from early April into May.
The massive slide created a natural dam across the Spanish Fork River, and the dam in turn created Thistle Lake, which completely submerged and destroyed the town of Thistle. The U.S. Corp of Engineers, the Utah National Guard, and construction workers from many companies joined UDOT workers in response to the Thistle slide. Efforts to control the slide turned to reconstruction of rail and roadways, and creation of a drainage tunnel to help bring down Thistle Lake.
Several years back I had the opportunity to participate in a collaborative effort with fellow archivists from USU and SUU to build an online exhibit of various records and record collections relating to the history along Highway 89. One of my contributions was a collection of photographs of the Thistle disaster, taken in real time by the Utah Department of Transportation’s staff photographer. Recently I revisited that online exhibit and curated some photos that document the disaster as it was unfolding. Enjoy!