Echoes of Lake Bonneville

Echoes of Lake Bonneville: North Spring, Fish Springs National Wildlife Refuge, Utah. Courtesy Utah Geological Survey
North Spring, Fish Springs National Wildlife Refuge, Utah. Courtesy Utah Geological Survey

Leland Harris wetlands, Snake Valley, Utah, Courtesy Utah Geological SurveyLeland Harris wetlands
Snake Valley, Utah
Courtesy Utah Geological Survey

Least Chub, Courtesy and Copyright Mark C. Belk, PhotographerLeast Chub
Courtesy & © Mark C. Belk, Photographer
Echoes of Lake Bonneville

Hi, I’m Holly Strand of the Quinney College of Natural Resources at Utah State University.

Deserts are dry by definition receiving an average of less than 10 inches of precipitation a year. In Utah’s cold West Desert, this skimpy amount of moisture slakes the thirst of sagebrush, saltbush or greasewood, but not much else. However, just like the Sahara, the West Desert has its oases. In certain lowland valleys you’ll find complexes of pools and marshes. There isn’t enough rain to form these freshwater sanctuaries. The water comes from giant underground aquifers.

Underneath the West Desert, the aquifer system acts as a storehouse for runoff from the surrounding mountains. As rainwater or snow melt enters or “recharges” the aquifer system, water pressure can build up in some areas. This pressure moves water through cracks and tunnels within the aquifer, and sometimes this water flows out naturally in the form of springs.

These desert springs–and the resulting pools and marshes–permit concentrations of animals and plants not possible under normal desert conditions. You’ll find sedges, rushes cattails and many other wetland plants. Both migratory and year round birds congregate here. There are even a couple of frog species—the Colombian spotted frog and the northern leopard frog.

But most remarkable are the desert spring residents that have survived from the days when the West Desert formed the floor of giant Lake Bonneville. Surveys have revealed a number of relict snails and other mollusks that still persist from that time. Some, like the Black Canyon Pyrg exist at a single spring complex only; they are found nowhere else on earth.

Certain native fish were also left high and dry by Lake Bonneville’s recession. The least chub is a good example. Now the sole member of its genus, this 3-inch long survivor is an unassuming but attractive little minnow. It is olive-colored on top and sports a gold strip on its steel-blue sides. It swims in dense but orderly schools in either flowing or still water. It can withstand both temperature variations and high salinity. The ability to tolerate different physical conditions has undoubtedly helped the least chub survive the post-Lake Bonneville millennium. Even so, the least chub was hanging on in only six different locations until Utah’s Division of Wildlife Resources reintroduced it to several more sites within its historic range. The Division and its conservation partners are still working to reduce threats to the least chub, to other spring residents and to the spring habitats themselves.

For more information and pictures go to www.wildaboututah.org

Thanks to Chris Keleher of Utah’s Department of Natural Resources for his help in developing this Wild About Utah story.

For Wild About Utah, I’m Holly Strand.

Credits:

Theme: Courtesy & Copyright Don Anderson Leaping Lulu
Image: Least Chub, Mark C. Belk, Professor of Biology, Brigham Young University
Image: Wetlands, Courtesy Utah Geological Survey https://geology.utah.gov/
Text: Holly Strand, Quinney College of Natural Resources at Utah State University

Sources & Additional Reading

Bailey, Carmen L., Kristine W. Wilson Matthew E. Andersen. 2005. CONSERVATION AGREEMENT AND STRATEGY FOR LEAST CHUB (IOTICHTHYS PHLEGETHONTIS) IN THE STATE OF UTAH Publication Number 05-24 Utah Division of Wildlife Resources a division of Utah Department of Natural Resources https://wildlife.utah.gov/pdf/fish/least_chubs.pdf

Jones, Jennifer, Rich Emerson, and Toby Hooker. 2013. Characterizing Condition in At-risk
Wetlands of Western Utah: Phase I UTAH GEOLOGICAL SURVEY a division of Utah Department of Natural Resources,https://geodata.geology.utah.gov/pages/view.php?ref=8364

Nature Serve entry for Least Chub: https://explorer.natureserve.org/servlet/NatureServe?searchName=Iotichthys+phlegethontis

Hanks, Joseph H. and Mark C. Belk. 2004. Threatened fishes of the world: Iotichthys phlegethontis Cope, 1874 (Cyprinidae) in Environmental Biology of Fishes, Vol. 71. N. 4., Kluwer Academic Publishers. https://dx.doi.org/10.1007/s10641-004-1030-x

Sigler W. F. & J. W. Sigler. 1996. Fishes of Utah, A Natural History. University of Utah Press, Salt Lake City. 375 pp. https://www.amazon.com/Fishes-Utah-A-Natural-History/dp/0874804698

Wasatch Front Canyons Geologic Tour, Virtual Tour created from Published Booklet (pdf) Geologic Guide to the Central Wasatch Front Canyons, Utah Geological Survey, State of Utah, https://utahdnr.maps.arcgis.com/apps/MapTour/index.html?appid=5cf1570b998346d98478a5abd50bf096

Geologic guides to the central Wasatch Front Canyons, Utah Geological Survey, 2005, https://geology.utah.gov/popular/utah-landforms/virtual-tour-central-wasatch-front-canyons/ [updated January 2024]

Til Death Do Us Part

Tundra Swan Pair
Cygnus columbianus
Courtesy US FWS
Tim Bowman, Photographer

Hi, I’m Holly Strand.

Each year we celebrate Valentine’s Day by expressing our love and devotion to a significant other. While humans are the only species that actually celebrate it, we aren’t the only animals who bond together as couples. Monogamy–or long term pair bonding as animal behaviorists call it–is practiced by over 90 % of birds. Along with a modest number of mammals, including wolves, beavers, voles and gibbons. Even a few fish pair up.

Monogamy may have evolved for different reasons among different groups of animals. For some, female dispersal may have played a role. If females are few and far between–as is the case with white tail ptarmigans–there is a tendency to pair up. Perhaps additional potential mates are too far away too bother. For males, monogamy can save a lot of time and energy. Monogamous males don’t have to fight over females or bother with first time courtship rituals. And by closely guarding a single female , males can protect their genetic investment.

There are advantages for females too. With a mate, you can get a little assistance around the nest or den. Male partners can help incubate eggs, guard against predators and help feed the kids. The fact that male and females are equally suited to care for chicks may explain why monogamy is so much more common among birds. The male improves his chances for reproductive success by investing in just one female’s little ones. The situation is different in mammals. Mammal males just can’t step in and help as much with gestation and lactation. So perhaps that’s why only 3% of mammal species form pair bonds.

The offspring of monogamous pairs tend to be pretty helpless at birth. Having two caregivers means that the you can take more time to mature. This long, slow development leads to larger brain sizes. Humans demonstrate this phenomenon very well as we parent our children longer than any other species on earth!

The tundra swan is Utah’s best example of monogamy in the wild. Young tundra swans date around a bit when they are young, but they eventually settle down with a single mate for life. They build and defend a nest together and raise the kids. But then they stick together the rest of the year as well. Greetings and courtship rituals such as head bobbing and dipping and ritual bathing strengthen their commitment toward each other.

You can see these beautiful swans in massive numbers twice a year when they migrate through Utah. Tens of thousands of them stop by the Great Salt Lake on their way to either the Arctic tundra or to central California.

For sources, pictures, and archives of past programs, go to www.wildaboututah.org

For Wild About Utah, I’m Holly Strand.

Credits:

Image: Courtesy US FWS, images.fws.gov
Text: Holly Strand

Sources & Additional Reading

Limpert, R. J. and S. L. Earnst. 1994. Tundra Swan (Cygnus columbianus), The Birds of North America Online (A. Poole, Ed.). Ithaca: Cornell Lab of Ornithology; Retrieved from the Birds of North America Online: https://bna.birds.cornell.edu/bna/species/089

Mocka, Douglas, and Masahiro Fujiokab. 1990. “Monogamy and long-term pair bonding in vertebrates” Trends in Ecology & Evolution. Volume 5, Issue 2, February 1990, Pages 39–43

Reichard, Ulrich and Christoph Boesch. 2003. Monogramy: mating Strategies and Partnerships in Birds, Humans and Other Mammals. Cambridge University Press.

Schultz, Susanne and Robin I.M. Dunbar. 2010. “Bondedness and sociality”
Behaviour, Volume 147, Number 7, 2010 , pp. 775-803(29).

Schultz, Susanne and Robin I.M. Dunbar. 2010. Social bonds in birds are associated with brain size and contingent on the correlated evolution of life-history and increased parental investment. Biological Journal of the Linnean Society. Volume 100, Issue 1, pages 111–123, May 2010.

Those Howling East Winds

Those Howling East Winds: Normal Diurnal Wind Shift Along the Wasatch Front, Courtesy Utah Division of Air Quality
Normal Diurnal Wind Shift
Along the Wasatch Front
Courtesy Utah Division of Air Quality

Those Howling East Winds: Air Pressure at the Surface, A Bit of a Blow..., Utah Climate Notes, January 2012, Courtesy Utah Climate Center, Utah State University Air Pressure at the Surface, 1 Dec 2011
Blue=Low Pressure, Red=High Pressure
The spacing of the lines is a measure of the pressure gradient: the closer the lines, the higher the pressure gradient. https://climate.usurf.usu.edu/news/010512Utah%20Climate%20Update%20(Jan%2012).pdf[Feb 6, 2014]
Read: A Bit of a Blow…
Courtesy Utah Climate Center, Utah State University

Wind is inevitable on a spinning planet with an atmosphere and a sun. At our latitude, westerlies prevail, but east winds do occur now and then. Locally, canyons daily exhale denser, cooler mountain air that drains into valleys. In Logan, trees blown by these canyon winds tilt westward. Occasionally, though, the whole Wasatch front is whipped by howling gales from the east, leaving behind shredded shingles, snapped tree limbs and rolled tractor-trailers. These forceful east wind events have a regional weather origin that is intensified by local topography.

It begins with a strong high-pressure cell parked over southwestern Wyoming.  It’s descending dry air circulates clockwise. Somewhere to the south or southwest, a low-pressure cell is needed.  The strong air pressure gradient between high and low generates a wind that races westward from Wyoming. The surging wind pours over the entire Wasatch front like water over a flat boulder in rapids.  These winds then plunge down slope, blowing quickest where the descent is long, steep, and unobstructed. The down rushing air slams onto the flat benches and valley floors.  In November 2011, such winds ripped Centerville with 100 MPH gusts.

Where these so-called mountain wave events blow regularly they often have names.  The mistral and foehn winds howl down from the Alps, chinooks  race down the Rocky Mountain Front Range, and the Santa Anas blast Southern California. The steep altitudinal descent of these parched winds compressively heats the air. A spark or flame soon transforms to a raging wildfire when fanned by a drying foehn or Santa Ana wind.  Europe’s foehns are also known to spark short tempers and stress.

Perhaps the sporadic easterly gales that lash the Wasatch Front and Cache Valley deserve an evocative name too.  For now, you at least know the answer to what’s blowin’ in the east wind.

Thanks to Martin Schroeder at the Utah Climate Center for insights and the stream boulder analogy

This is Linda Kervin for Bridgerland Audubon Society.

Credits:
Diurnal Utah Winds Image: Courtesy Utah Division of Air Quality
Surface Air Pressure 1 Dec 2011 Image: Courtesy Utah Climate Center, USU
Text: Jim Cane

Additional Reading:

Martin Price, Alton Byers, Donald Friend, Thomas Kohler, Larry W. Price. 2013. Mountain Geography: Physical and Human Dimensions. Univ of California Press. pages 71­74. https://www.amazon.com/Mountain-Geography-Physical-Human-Dimensions/dp/0520254317

Mesmerizing live wind map of US at:  https://hint.fm/wind/

Forecast of damaging east winds along the Wasatch Front, end of November 2011, https://www.ksl.com/?sid=18282965

How Chinooks Occur, Wikipedia, https://en.wikipedia.org/wiki/Chinook_wind#How_Chinooks_occur

Citius, Altius, Fortius

Snowshoe Hare summer coat image courtesy US National Parks Service
Snowshoe Hare Summer Coat
Courtesy US National Parks Service

Snowshoe Hare winter coat image courtesy US Forest Service https://www.fs.fed.us Snowshoe Hare Winter Coat
Courtesy USDA Forest Service

Hi, I’m Holly Strand from the Quinney College of Natural Resources at Utah State University

The upcoming winter Olympics in Sochi bring back fond memories of Utah’s stint as host of the winter games. You may recall that “Powder,” a playful snowshoe hare was among Salt Lake City’s three Olympic mascots. Powder represented “faster” in the Olympic triumvirate (try-um-virate) motto of “Citius, Altius, Fortius” (or Faster, Higher Stronger). And the little snowshoe hare needs to be fast. For according to USU wildlife biologist Dustin Ranglack Snowshoe hares are the Snickers bars of the forest. They’re a popular treat for a host of carnivores, including coyotes, foxes, lynx, bobcats, bears and birds of prey.

Hares are fast in general. They can reach 40 miles per hour, and can leap more than ten feet (three meters). But this hare has extra-large, wide feet with more fur and larger toes. Like permanent snowshoes, these feet are ideally suited for racing from predators in deep mountain snow.

In spite of its speed, the snowshoe hare’s best mechanism of defense is camouflage. In winter, its soft, fine fur turns white to blend into the snowy terrain. As spring thaws the wintry landscape, the hare’s fur turns brown or reddish-brown to help it elude predators. Only the tips of the ears remain dark throughout the year.

Scientists have observed that climate change may affect the survival of animals that undergo seasonal coat color changes. For example, with a shortened winter, a white-coated snowshoe hare is a sitting duck on brown earth in full view of ravenous predators.

But interestingly there is already a lot of variability in the timing of individual hares camouflaged coat. Amount of sunlight may start the color change in a snowshoe hare population. But once the process starts, the timing of full coat transformation — which can take up to two months — is unique. Perhaps this is due to the fact that—even before climate change– there was always been some variability in the onset of winter snow cover. Anyway, this variability in color change gives scientists hope that the snowshoe hare will be able to adapt its timing to seasonal changes in the future.
For sources and pictures go to WWW.wildaboututah.org.

For the Quinney College of Natural Resources, I’m Holly Strand

Credits:

Images: Courtesy US Forest Service and US National Parks Service

Text: Mary-Ann Muffoletto, Holly Strand, Quinney College of Natural Resources

Sources & Additional Reading

Snowshoe Hare Lepus Americanus, National Geographic, https://animals.nationalgeographic.com/animals/mammals/snowshoe-hare.html

Mills, L. Scott, Marketa Zimovaa, Jared Oylerb, Steven Runningb, John T. Abatzoglouc, and Paul M. Lukacsa. 2013 Camouflage mismatch in seasonal coat color due to decreased snow duration. PNAS. https://www.pnas.org/content/early/2013/04/10/1222724110#aff-1

Rossner, Hillary. 2012. The Color of Bunny: Can snowshoe hares outrace climate change? Feb. 6, 2012. High Country News. https://www.hcn.org/issues/44.2/can-snowshoe-hares-adapt-to-climate-change