June 2014 - Wild About Utah

June 26, 2014January 5, 2024

Sandhill Cranes, Utah’s Meadow Dancers

Sandhill Crane Pair, Grus canadensis, Courtesy US FWS, Justine Belson, Photographer — Sandhill Crane Pair
*Grus canadensis*
Courtesy US FWS,
Justine Belson, Photographer

Cranes of the Swaner Nature Preserve by Michael Flaherty, Nesting cycle of Sandhills Cranes, Swaner Nature Preserve, Park City, UT

Hi, this is Mark Larese-Casanova from the Utah Master Naturalist Program at Utah State University Extension.

The grace of sandhill cranes draws our attention when we see them in the marshes, meadows, and fields across northern Utah. As one of the tallest birds in the state, the sandhill crane is hard to miss. They’ll glide low over farm fields, with their large slate-grey bodies and red caps making them difficult to mistake with any other bird.

Northern Utah is near the lower end of the sandhill crane’s breeding range, so we’re fortunate to see them. They’ll arrive to Utah beginning in March, and stay for the summer breeding season.

Sandhill cranes develop pair bonds for life, and their choice in mates is influenced by elaborate courtship dances. Crane dances are like awkward avian ballet, with an assortment of bows, flapping wings, and leaps into the air with wings outstretched. At times, sticks or plants are grasped with their long, dagger-like bills and tossed into the air. At up to four feet tall with a wingspan of five feet, the sandhill crane as it dances is quite a sight to see!

Sandhill cranes are often heard before they’re seen. Their loud, rolling trumpets fill the air, even for a couple miles. Males and females call in unison, as a loud duet that helps reinforce their pair bond.

Once a suitable nest location is found on the ground or on shallow water, both the male and female toss plant material over their shoulders to build their large nest. As spring now fades to summer, sandhill cranes can be seen strolling through farm fields with their young colts, encouraging them to feed, and protecting them from predators. While the dance of the sandhill cranes has mostly ended, their elegance hangs in our memory until next year.

As Aldo Leopold wrote in A Sand County Almanac, “our appreciation of the crane grows with the slow unraveling of earthly history… And so they live and have their being- these cranes- not in the constricted present, but in the wider reaches of… time. A crane marsh holds a paleontological patent of nobility, won in the march of aeons.”

For Wild About Utah, I’m Mark Larese-Casanova.

[End with Kevin Colver, WesternSoundscape.org sandhill crane call again https://collections.lib.utah.edu/details?id=1117102&q=sandhill+crane]

Credits:

Theme: Courtesy & Copyright Don Anderson Leaping Lulu
Images: YouTube video Courtesy and Copyright Michael Flaherty, Park City. UT
Audio: Copyright Kevin Colver
Text & Voice: Mark Larese-Casanova, Utah Master Naturalist Program at Utah State University Extension.

Additional Reading:

References:
Cornell Lab of Ornithology. Sandhill Crane. All About Birds. https://www.allaboutbirds.org/guide/sandhill_crane/lifehistory

Leopold, A. 1986. A Sand County Almanac. Ballantine Books. https://www.amazon.com/County-Almanac-Outdoor-Essays-Reflections/dp/B00J5SEZ6S

National Wildlife Federation. Sandhill Crane. https://www.nwf.org/wildlife/wildlife-library/birds/sandhill-crane.aspx

Tekiela, S. 2003. Birds of Utah. Adventure Publications, Inc. Cambridge, Minnesota. https://www.amazon.com/Birds-Field-Guide-Identification-Guides/dp/1647554071

Species, Utah Division of Wildlife Resources, Utah Department of Wildlife Resources. Sandhill Crane. https://fieldguide.wildlife.utah.gov/?species=antigone%20canadensis

US Geological Survey. Sandhill crane summer distribution map. https://www.mbr-pwrc.usgs.gov/bbs/htm96/map617/ra2060.html

Photos:
Category:Grus canadensis, Wikimedia Commons, https://commons.wikimedia.org/wiki/Category:Grus_canadensis#mediaviewer/File:Grus_canadensis,_two,_Bosque_del_Apache_NWR.jpg

Category:Grus canadensis, Wikimedia Commons, https://commons.wikimedia.org/wiki/Category:Grus_canadensis#mediaviewer/File:Sandhill_Crane_in_Love^_%28_Grus_canadensis_pratensis_%29_-_Flickr_-_Andrea_Westmoreland.jpg

A Sandhill Crane flying at Sacramento River National Wildlife Refuge, Dayton, California, USA., Courtesy USFWS, Steve Emmons, Photographer, https://commons.wikimedia.org/wiki/Category:Grus_canadensis_in_flight#mediaviewer/File:Grus_canadensis_-Sacramento_River_National_Wildlife_Refuge,_Dayton,_California,_USA_-flying-8.jpg

June 19, 2014June 26, 2016

Dust in the Wind

U.S. Geological Survey photo by Mark Miller — Dust Storm Milford Flats
4 March 2009
US Geological Survey photo by Mark Miller

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

American paleontologist Roy Chapman Andrews was a frequent visitor to the Gobi Desert. This is how he described being caught in a Gobi desert dust storm: “Seemingly a raging devil stood beside my head with buckets of sand, ready to dash them into my face…” “…after each raging attack it would draw off for a few moments’ rest. Then suddenly the storm devil was on us again, clawing, striking, ripping, seeming to roar in fury that any of the tents still stood.”

Andrews didn’t have to go so far to feel the rage of a dust storm. He could have come to western Utah. While we don’t have the monstrous storms of the Sahara and the Gobi/Manchurian deserts, the eastern Great Basin–which is essentially western Utah–sits secure on any global list of dust storm hotspots.

Let’s consider why this is so…

First and foremost, western Utah has the dust. In scientific terms, dust is any particle—organic or inorganic—that is less than .63 microns or smaller in diameter. .63 microns is about half the width of a single human hair. In geological terms think silt or clay particles. A grain of sand is much larger. If you are the size of a dust particle, then a relatively small puff of wind will release you into the air. And you’ll stay there until it’s completely calm or rain forces you down.

A great place to find geologic dust is in desert playas. For runoff sediments collect in these dry lake depressions. Western Utah has several of these desert dust bins. And satellite data have confirmed that playas such as Sevier Dry Lake, Tule Dry Lake, and Great Salt Lake Desert are major sources of dust plumes. The alluvial fans of the Great Basin mountains provide an additional source of dust.

To get this dust airborne you need wind which is also plentiful in western Utah. This region typically experiences strong south and southerwesterly winds called “hatu winds.” That’s Utah spelled backwards. The name was coined by colorful Utah meteorologist Mark Eubank. These hatu winds blow south to north or to the northwest. They pick up speed and dust as they race along the north-south trending Great Basin ridges. They can reach speeds of over 90 miles per hour.

Utah’s hatu winds peak in the spring months with a secondary peak in August-September. In spring these windy freight trains full of dust can hit the populated Wasatch Front wreaking havoc with air quality and human health.

Sometimes raindrops capture dust in the airstream and splat them onto our windshields and windows. These mud rains are most common in spring when the hatus are at their peak. And this is why saavy Utahns never bother washing their home windows until June.

While dust storms can be considered natural events, the fact that they are increasing in number and severity is definitely unnatural. The increase is caused by human-related activities that remove vegetation or break the biological soil crusts that help stabilize dust and soil. Overgrazing, water withdrawals, military operations, farming on marginal lands, off-road vehicle riding, fires, even restoration activities all release dust to be carried off by the next significant wind.

Thanks to Atmospheric Scientist Maura Hahnenberger for her help with this Wild About Utah story.

For Wild About Utah, and the Quinney College of Natural Resources, I’m Holly Strand.

Credits:

Images: Courtesy USGS.gov and NRCS.gov
Sound: Wind sound effect from Sound Bible.com Recorded by Mark DiAngelo https://soundbible.com/1810-Wind.html
Text: Holly Strand

Sources & Additional Reading

Hahnenberger, M. and K. Nicoll. Geomorphic and land use characteristics of dust sources in the eastern Great Basin of Utah, U.S.A. Accepted Geomorphology.

Hahnenberger, M. and K. Nicoll, 2012. Meteorological characteristics of dust storm events in the eastern Great Basin of Utah, U.S.A. Atmospheric Environment, 60, 601-612.

Jason P Field, Jayne Belnap, David D Breshears, Jason C Neff, Gregory S Okin, Jeffrey J Whicker, Thomas H Painter, Sujith Ravi, Marith C Reheis, and Richard L Reynolds The ecology of dust Front Ecol Environ 2010; 8(8): 423–430, doi:10.1890/090050 (published online 12 Oct 2009)https://www.esajournals.org/doi/pdf/10.1890/090050

Neff, J. C., A. P. Ballantyne, G. L. Farmer, N. M. Mahowald, J. L. Conroy, C. C. Landry, J. T. Overpeck, T. H. Painter, C. R. Lawrence, and R. L. Reynolds, 2008: Increasing eolian dust deposition in the western United States linked to human activity. Nature, 1, 189-195

Warner, Thomas T. 2004. Desert Meteorology. NY: Cambridge University Press

Washington, R., M. Todd, N. J. Middleton and A. S. Goudie, 2003. Dust-storm source areas determined by the Total Ozone Mapping Spectrometer and Surface Observations, Annals of the Association of American Geographers, 93(2), 297-313.

Miller, M. E., et al. (2012). “Post-fire land treatments and wind erosion – Lessons from the Milford Flat Fire, UT, USA.” Aeolian Research 7: 29-44.

Steenburgh, W. J., et al. (2012). “Episodic Dust Events of Utah’s Wasatch Front and Adjoining Region.” Journal of Applied Meteorology and Climatology 51(9): 1654-1669.

June 12, 2014July 18, 2020

National Park or National Monument?

Established in 1916 the National Park Service manages all properties included in the National Park System. This system includes over 400 areas that encompass more than 84 million acres of land. These areas can go by one of 31 different titles. Within this system, Utah boasts 1 national historic site, 2 national recreation areas, 7 national monuments, and 5 national parks. While the reason for some of these titles is self-explanatory, the reason for others is less clear. National Park or National Monument?

For example, what makes one area a “national park” and another a “national monument?” Most people – including myself – would probably guess that the difference is in size. And while this is sometimes true, the primary difference is the reason for which each is established, because these two designations grew from historically separate concepts. The notion of the national park, which was simply the idea of large-scale natural preservation for public enjoyment, grew in popularity throughout the 1800s. As a result you can typically think of a national park as a spectacular scenic feature or natural phenomena preserved for inspirational, educational, and recreational value.

On the other hand, the idea of the national monument arose as a result of the need and desire to also protect prehistoric cliff dwellings, pueblo remains, and other historic ruins found by explorers of the American West and Southwest. Efforts to protect these sites resulted in the passing of the Antiquities Act of 1906. Therefore a national monument is usually designated to preserve objects of prehistoric, historic, cultural, and/or scientific interest. However, the Antiquities Act has been used more widely to preserve natural features as well, meaning the content of national monuments can be quite varied from wilderness areas to military sites to buildings and ruins.

There are also a couple of legal differences between these two designations. National parks are established through acts of Congress, whereas national monuments are established by Presidential proclamation. Administratively, the National Park Service manages all national parks. While national monuments, depending on their location and content, can fall under not only under the jurisdiction of the National Park Service, but also that of the U.S. Forest Service, the U.S. Fish and Wildlife Service, the National Oceanic and Atmospheric Administration, the Department of Defense, or the Bureau of Land Management.

So, it’s not just size that makes the difference, its intent, content, process of establishment, and administration. The next time you visit one of Utah’s national parks or monuments, will you be able to tell the difference?

For Wild About Utah, I’m Anna Bengtson of Park City.

Arches National Park
Bryce Canyon National Park
Capitol Reef National Park
Canyonlands National Park
Zion National Park

Golden Spike National Historic Site
Cedar Breaks National Monument
Dinosaur National Monument
Grand Staircase National Monument
Hovenweep National Monument
Natural Bridges National Monument
Pipe Spring National Monument(Border Utah/Arizona)
Rainbow Bridge National Monument
Timpanogos Cave National Monument

Flaming Gorge National Recreation Area
Glen Canyon National Recreation Area

Credits:
Image: Courtesy and Copyright Anna Bengston
Text: Anna Bengston

Additional Reading:

Biggers, Ashley. “National Parks Versus National Monuments.” Outside Online. 22 Apr. 2014. Web. 8 June 2014. https://www.outsideonline.com/adventure-travel/escapes/travel-agent/The-Difference-between-National-Parks-and-National-Monuments.html.

McDonnell, Janet. The national parks: shaping the system. 3rd ed. Washington, D.C.: U.S. Dept. of the Interior, 2005. Web, 8 June 2014. https://www.nps.gov/parkhistory/online_books/shaping/index.htm.

O’Connor, Mary. “Killing A Bill that Could Save National Parks.” Outside Online. N.p., 14 Apr. 2014. Web. 8 June 2014. https://www.outsideonline.com/outdoor-adventure/the-current/footprint/Five-Treasures-We-Owe-to-the-Imperiled-Antiquities-Act.html.

“Parks and Monuments.” Utah. N.p., n.d. Web. 8 June 2014. https://www.visitutah.com/parks-monuments/.

Righter, Robert. “National Monuments to National Parks:
The Use of the Antiquities Act of 1906”, National Park Service History: National Monuments to National Parks. N.p., Aug. 1989. Web. 8 June 2014. https://www.nps.gov/parkhistory/hisnps/npshistory/righter.htm.

United States. National Park Service. “National Park Service History: National Park System Nomenclature.” National Parks Service. U.S. Department of the Interior, n.d. Web. 8 June 2014. https://www.nps.gov/history/history/hisnps/NPSHistory/nomenclature.html.

United States. National Park Service. “Frequently Asked Questions.” National Parks Service. U.S. Department of the Interior, 28 May 2014. Web. 8 June 2014. https://www.nps.gov/faqs.htm.

Yard, Robert Sterling, and Isabelle F. Story. “Parks vs. Monuments.” The national parks portfolio. 6th ed. Washington: U.S. Government Printing Office, 1931. Web, 8 June 2014. https://www.nps.gov/history/history/online_books/portfolio/portfolio0b.htm.

June 5, 2014December 4, 2023

Gardening for Hummingbirds

At long last, summer has returned as have the hummingbirds who zip around my garden, visiting flowers and chasing off intruders. (Kevin Colver: Songbirds of Rocky Mountain Foothills. Broad-tailed Hummingbird) Hummingbirds are a delight in the yard and so we plant flowers specifically to attract and feed them. In general, hummingbirds prefer long tubular flowers especially those that are red, orange or violet. But not all these flowers are created equally.Gardening for Hummingbirds

Hummingbirds visit flowers for their nectar which fuels their flight. Their long tongue reaches well beyond the tip of their needle like bill when they lap up nectar; capillary action then draws the sweet liquid up tiny grooves along the length of the tongue.

Floral nectar evolved to attract potential pollinators. The floral nectary is generally found inside the flower, at the base. When probing for nectar, floral visitors brush by the reproductive structures. Pollen adheres to parts of their body and then at the next flower of the same species, some pollen sticks to the female stigma. This transfer is pollination.

Many nectar-rich flowers grow well in Utah gardens. In the xeric garden, Penstemons are a good choice, as are Red Hot Pokers and Zauschneria, sometimes called Hummingbird Trumpet. In more moist sites, red flowered Heuchera is popular. Some red flowered cacti and Trumpet Creeper are good choices, as are Agastache and many Salvias.

Watch which flowers hummers visit. They will check out many blooms, but the ones they routinely return to are the ones yielding generous nectar. Many flowers produce little or no nectar, including some that look to us like good hummingbird flowers. Also, many horticultural hybrids and doubled flowers produce paltry amounts of nectar.

To encourage hummingbirds to remain in your garden, you can grow trees and shrubs for cover. Nectar is only part of their diet. For protein, they regularly eat insects and spiders small enough for their tiny bill so a garden free of insects is not desirable. They also appreciate a place to perch where they can digest, wait for a tasty insect to fly by and keep an eye out for potential rivals. So grab your trowel and lets feed those hummers.(Kevin Cover: Songbirds of Rocky Mountain Foothills. Broad-tailed Hummingbird)

This is Linda Kervin for Bridgerland Audubon Society.

Credits:

Images: Courtesy and Copyright Jim Cane, Photographer
Theme: Courtesy & Copyright Don Anderson as performed by Leaping Lulu
Text & Voice: Linda Kervin, Bridgerland Audubon Society

Additional Reading:

Linda Kervin’s pieces on Wild About Utah

Hummingbirds and How to Attract Them, Washington Department of Fish & Wildlife, https://wdfw.wa.gov/living/hummingbirds/

Hummingbirds 101, The Hummingbird Society, https://www.hummingbirdsociety.org/hummingbirds-101/

Coro Arizmendi Arriaga, Maria del, Hummingbirds of
Mexico and North America, In Spanish and English, CONABIO, 2014, https://www.biodiversidad.gob.mx/Difusion/pdf/colibries_mexico_y_norteamerica.pdf

Gardening for Hummingbirds
Gardening for Hummingbirds
Gardening for Hummingbirds