Tag Archive for: utah

The “Glad You Asked” article, What is the correct name of…?, in a previous issue of Survey Notes addressed how to find the correct names of Utah’s geographic features using the U.S. Geological Survey’s Geographic Names Information System (GNIS).

This article addresses how to propose a new name or change an existing geographic feature name.

Policies for naming geographic features have been established by the Domestic Names Committee (DNC) of the U.S. Board on Geographic Names. Want to name a geographic feature after your boss or favorite geologist? First, wait until they have been deceased five years as features cannot be named after the living or recently deceased.

Additionally, they need to have had a direct and long-term association with the feature (tragic death at a site does not normally qualify). Exceptions are made for those who have made a significant contribution to the area or state and those “with an outstanding national or international reputation.”

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Plants can enlighten geologists as to the rock beneath. Geobotany, also called phytogeography, is the scientific study of the distribution of plants.

Climate is considered the primary control on plant life, but within a particular climatic region the rock beneath soil—known as the parent material of soil—is typically the key factor influencing the vegetation growing above. Rock ultimately determines soil moisture characteristics, nutrient availability, and concentrations of essential elements.

Therefore, certain plants are associated with specific rock types. Limestone, dolomite, shale, gypsum, chert, gabbro, rock salt, and ultramafic rocks (e.g., dunite, peridotite, serpentinite), for example, are known for their distinctive floras. Since before the advent of agriculture humans have used plants as a guide to find sought-after rocks and minerals. Today, the methodologies of geobotany are still applicable, practical, and even cost-effective to the geologist.

Dramatic changes in vegetation can occur with changes in geology. In mountain ranges of the Great Basin, big sagebrush growing on sandstone abruptly transitions to bristlecone pine on dolomite. The distribution of the California poppy in Arizona closely correlates with copper mineralization, which in turn corresponds with fault lines.

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Among the more commonly asked questions we receive at the Utah Geological Survey (UGS) are those dealing with the correct names of Utah’s geographic features.

Perhaps the best tool for answering these questions is a searchable database established and maintained by the U.S. Board on Geographic Names, which is part of the U.S. Geological Survey (USGS). This database, called the Geographic Names Information System (GNIS), is available online at geonames.usgs. gov.

Following the American Civil War, a surge of exploration, mining, and settlement of western territories created many inconsistencies and contradictions in geographic names, which became a serious problem for surveyors, map makers, and scientists.

To address this problem, President Benjamin Harrison signed an executive order that created the U.S. Board on Geographic Names in 1890 (the current form of the board was established by a 1947 law). Technology, such as geographic information systems, global positioning systems, and the Internet increases the need for standardized data on geographic names, but it also makes accessing that data quick and easy through the GNIS.

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Digging in the dirt does not sound like a glamorous job, but it caught the attention of the cable television network’s Discovery Channel.  The show, DIRTY JOBS recently went on a dinosaur dig with some paleontologists from the Utah Geological Survey (UGS).  The show is set to air on Tuesday, December 20.

According to the show’s website:  “DIRTY JOBS profiles the unsung American laborers who make their living in the most unthinkable — yet vital — ways. Our brave host and apprentice Mike Rowe introduces you to a hardworking group of men and women who overcome fear, danger and sometimes stench and overall ickiness to accomplish their daily tasks.”

State Paleontologist Jim Kirkland and UGS paleontologist Don DeBlieux traveled with the cast and crew of the show to an undisclosed location in eastern Utah for the one day shoot to look for and dig dinosaur bones out of the side of a steep hill.  “We picked that site because it is such a spectacular location, but it is a difficult location and one which requires lots of hard and strenuous work,” says DeBlieux.

In fact, the weather was very uncooperative as they were driving to the site.  “It rained for a couple of hours in the morning and we were afraid that we weren’t going to be able to film, and they only had one day to shoot.  But luckily, the skies cleared and it turned out to be a nice day.”  The show points out that you have to have patience, strength and a love of playing in the dirt in order to be a paleontologist.

“We are excited to see the show because we have only seen the trailers,” said DeBlieux.  “But based on the trailers, it should be pretty amusing!”

Some of the episode’s trailers can be seen at: http://dsc.discovery.com/videos/dirty-jobs-sneak-peek/

The Utah Geological Survey provides timely scientific information about Utah’s geologic environment, resources, and hazards.

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Heads up, map geeks! (We know you’re out there.)

The Utah Geological Survey has released a full-color geological map of unprecedented detail of 1,800 square miles of the central Wasatch, which includes wilderness areas and public lands along with human-infested areas, including Heber and Payson.

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The Utah Geological Survey has released its 2012 Calendar of Utah Geology. Of the more than 300 photos that were submitted, 33 were selected for the 2012 calendar.

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The Utah Geological Survey has released its 2012 Calendar of Utah Geology. Of the more than 300 photos that were submitted, 33 were selected for the 2012 calendar.

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GET IT HERE

Near the town of Echo in northern Utah is a cluster of reddish-brown natural monuments called The Witches (also known as Witch Rocks, Witches Rocks, Witch Bluffs, or Witches Bluffs), composed of the Echo Canyon Conglomerate.

In 1858, army Captain Albert Tracy described them in his journal as “witch-like” and “so singularly like figures in kirtles [long skirts] and steeple-hats, or bonnets that they have received the appellation [Witch Rocks]”. By using your imagination (and perhaps squinting a bit), you can picture a coven of witches in long robes and witches’ hats standing on the hillside.

Nearby Echo Canyon has long been used as a main thoroughfare between southern Wyoming and northern Utah, first by Native Americans, fur trappers, and explorers, then by wagon trains on their way to Salt Lake City or other points west. Before the interstate highway, passengers on the Overland Stage and then the Union Pacific Railroad also made their way through the canyon.

At the town of Echo, the canyon opens into the Henefer Valley where most of these travelers rested and marveled at the unusual rock formations, some even drawing sketches or taking photographs of The Witches.

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Insurance companies have given no help to some North Salt Lake residents whose homes are being destroyed by a slow-moving landslide. Nor has the federal government. But their neighbors did on Saturday — rallying with a community breakfast and fun run to raise money to help.

“I’m glad somebody — somebody — is helping. We need it,” said Stefanie Christiansen, whose home is being torn apart slowly. She, like many of her neighbors on Springhill Circle and Springhill Drive, were among the volunteer cooks and servers Saturday during the breakfast at Foxboro Regional Park.

As she was helping serve hot pancakes to neighbors paying $5 each, she said, “We really appreciate what people are doing for us. It means a lot.”

She said she and her husband bought their house on Springhill Drive in the foothills 15 years ago.

“Then in 1998, we had some movement from the landslide. Then it was fine for a lot of years,” she said. But more recently, it started moving again — about an inch a year — cracking foundations and walls, and tearing apart homes.

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The recent rains have caused more than a fear of flooding, as canyon hillsides are threatening to collapse and roads are being covered with mud.

“We’ve had this continuous rainfall that really started back in October,” said Jeff Niermeyer, Salt Lake City Public Utilities director. “It has just rained and rained and there’s no place for the water to go.”

The hillside at the mouth of City Creek Canyon, he said, has been sliding under increased water pressure since 1937, but has already moved 8 feet this spring with all the recent moisture.

“It starts to saturate the upper surface of the groundwater and what that does is basically relieve the inner pressure between the soil particles and creates the potential for landslides,” Niermeyer said.

Excess water sent an estimated 200,000 tons of rocks and mud onto state Route 39 Thursday evening, damaging at least two cars and closing the road on the southern shores of Pineview Reservoir for most of the day. Utah Department of Transportation engineer Brent DeYoung said the hillside had been stabilized, but more rain could change that.

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