NV5 Geospatial has mapped more than 26 million acres of North America’s shoreline and riverine environments across more than 200 projects.
The projects have spanned from the Nuyakuk River in Alaska, Lake Tahoe in California, the Rio Grande in Texas, the entire coasts of South and North Carolina, the Achigan River in Quebec, Chesapeake Bay in Maryland and the Florida Keys.
In 2022, the company mapped and acquired topobathymetric lidar data for 14 projects including the Yellowstone River, Wyoming; Hells Canyon, Indiana; Revillagigedo Island, Alaska and Iles de la Madeleine in Quebec.
NV5 Geospatial first mapped these environments in 2012 using high-resolution bathymetric lidar and natural color imagery. The company mapped 34,051 acres of shoreline along the Sandy River, located in northwestern Oregon, to study the ever-changing basin geomorphology.
NV5 has also signed a two-year contract with the National Geodetic Survey of the National Oceanic and Atmospheric Administration to provide topobathymetric lidar, 4-band imagery and mapping of 3,115 sq miles of the Maine shoreline.
“For a decade we have been helping local, state, and federal government agencies as well as commercial and private entities gain the insights they need to solve some of their most challenging nearshore and riverine projects through our mapping technologies including topobathymetric lidar,” Kurt Allen, vice president of NV5 Geospatial, said. “Whether it be mapping the shoreline after a hurricane, updating the national shoreline, assisting water boards with flood planning, or hundreds of other possible use cases, we are constantly improving our technology and scalability to always be at the ready for our customers.”
Old Faithful is Yellowstone National Park’s most famous landmark. Millions of visitors come to the park every year to see the geyser erupt every 44 to 125 minutes. But despite Old Faithful’s fame, relatively little was known about the geologic anatomy of the structure and the fluid pathways that fuel the geyser below the surface. Until now.
University of Utah scientists have mapped the near-surface geology around Old Faithful, revealing the reservoir of heated water that feeds the geyser’s surface vent and how the ground shaking behaves in between eruptions. The map was made possible by a dense network of portable seismographs and by new seismic analysis techniques. The results are published in Geophysical Research Letters. Doctoral student Sin-Mei Wu is the first author.
For Robert Smith, a long-time Yellowstone researcher and distinguished research professor of geology and geophysics, the study is the culmination of more than a decade of planning and comes as he celebrates his 60th year working in America’s first national park.
“Here’s the iconic geyser of Yellowstone,” Smith says. “It’s known around the world, but the complete geologic plumbing of Yellowstone’s Upper Geyser Basin has not been mapped nor have we studied how the timing of eruptions is related to precursor ground tremors before eruptions.”
A portable seismometer used to map the geology beneath Old Faithful. (Photo: Paul Gabrielsen)
Small seismometers
Old Faithful is an iconic example of a hydrothermal feature, and particularly of the features in Yellowstone National Park, which is underlain by two active magma reservoirs at depths of 5 to 40 km depth that provide heat to the overlying near-surface groundwater. In some places within Yellowstone, the hot water manifests itself in pools and springs. In others, it takes the form of explosive geysers.
Dozens of structures surround Old Faithful, including hotels, a gift shop and a visitor’s center. Some of these buildings, the Park Service has found, are built over thermal features that result in excessive heat beneath the built environment. As part of their plan to manage the Old Faithful area, the Park Service asked University of Utah scientists to conduct a geologic survey of the area around the geyser.
For years, study co-authors Jamie Farrell and Fan-Chi Lin, along with Smith, have worked to characterize the magma reservoirs deep beneath Yellowstone. Although geologists can use seismic data from large earthquakes to see features deep in the earth, the shallow subsurface geology of the park has remained a mystery, because mapping it out would require capturing everyday miniature ground movement and seismic energy on a much smaller scale. “We try to use continuous ground shaking produced by humans, cars, wind, water and Yellowstone’s hydrothermal boilings and convert it into our signal,” Lin says. “We can extract a useful signal from the ambient background ground vibration.”
To date, the University of Utah has placed 30 permanent seismometers around the park to record ground shaking and monitor for earthquakes and volcanic events. The cost of these seismometers, however, can easily exceed $10,000. Small seismometers, developed by FairfieldNodal for the oil and gas industry, reduce the cost to less than $2,000 per unit. They’re small white canisters about six inches high and are totally autonomous and self-contained. “You just take it out and stick it in the ground,” Smith says.
In 2015, with the new instruments, the Utah team deployed 133 seismometers in the Old Faithful and Geyser Hill areas for a two-week campaign.
The sensors picked up bursts of intense seismic tremors around Old Faithful, about 60 minutes long, separated by about 30 minutes of quiet. When Farrell presents these patterns, he often asks audiences at what point they think the eruption of Old Faithful takes place. Surprisingly, it’s not at the peak of shaking. It’s at the end, just before everything goes quiet again.
After an eruption, the geyser’s reservoir fills again with hot water, Farrell explains. “As that cavity fills up, you have a lot of hot pressurized bubbles,” he says. “When they come up, they cool off really rapidly and they collapse and implode.” The energy released by those implosions causes the tremors leading up to an eruption.
One scientist’s noise is another scientist’s signal
Typically, researchers create a seismic signal using an active source, such as swinging a hammer onto a metal plate on the ground or setting off an explosion. Lin and Wu developed the data analysis method that would help find useful signals among the seismic noise without disturbing the sensitive environment in the Upper Geyser Basin. Wu says she was able to use the hydrothermal features themselves as a seismic source, to study how seismic energy propagates by correlating signals recorded at the sensor close to a persistent source to other sensors. “It’s amazing that you can use the hydrothermal source to image the structure here,” she says.
The model of Old Faithful’s hydrogeological system suggested by the study’s results. (Image: Sin-Mei Wu)
When analyzing data from the seismic sensors, the researchers noticed that tremor signals from Old Faithful were not reaching the western boardwalk. Seismic waves extracted from another hydrothermal feature in the north slowed down and scattered significantly in nearly the same area suggesting somewhere west of Old Faithful was an underground feature that affects the seismic waves in an anomalous way. With a dense network of seismometers, the team could determine the shape, size, and location of the feature, which they believe is Old Faithful’s hydrothermal reservoir.
Wu estimates that the reservoir, a network of cracks and fractures through which water flows, has a diameter of around 200 meters, a little larger than the University of Utah’s Rice-Eccles Stadium, and can hold approximately 300,000 cubic meters of water, or more than 79 million gallons. By comparison, each eruption of Old Faithful releases around 30 m3 of water, or nearly 8,000 gallons. “Although it’s a rough estimation, we were surprised that it was so large,” Wu says.
Further work
The team is far from done answering questions about Yellowstone. They returned for another seismic survey in November 2016 and are planning their 2017 deployment, to begin after the park roads close for the winter. Wu is looking at how subsurface structure and hence the propagation of seismic waves can change with time. Farrell is using the team’s seismic data to produce even higher resolution subsurface images and predict how earthquake waves might reverberate through the region.
Smith is looking forward to conducting similar analysis in Norris Geyser Basin, the hottest geothermal area of the park. Lin says that the University of Utah’s research program in Yellowstone owes much to Smith’s decades-long relationship with the park, enabling new discoveries. “You need new techniques,” Lin says, “but also those long-term relationships.”
The full study can be found here. The research was funded by the National Science Foundation and by King Abdullah University of Science and Technology, the Brinson Foundation and the Carrico Fund. Fan-Chi Lin is the Principal Investigator.
Paul Gabrielsen is a science writer at University of Utah Communications.
On the 100th anniversary of National Geographic’s Cartographic Division, National Geographic Maps will make available hundreds of maps from its Trails Illustrated line through Avenza Systems Inc.’s PDF Maps app.
The addition of these outdoor recreation maps in North America augments the PDF Maps app digital map database by incorporating trail maps. It also increases National Geographic Maps’ reach within the mobile consumer market, giving more consumers access to the Trails Illustrated line. Trail maps from many of America’s national parks have already been uploaded to the app, including Yosemite, Yellowstone, Grand Teton, Zion and Great Smoky Mountains.
With many Ranger Districts throughout the country discontinuing visitor services, Avenza’s PDF Maps app provides an alternative for outdoor enthusiasts planning a trip in remote areas where Internet service is not always available to stream detailed map content. Using National Geographic’s line of detailed recreation maps, PDF Maps app users can purchase, download and save maps on GPS-enabled devices such as Android- and iOS-based phones and tablets. Park visitors can use the app to find and mark location directly on the downloaded National Geographic map. Features include location tagging, dropping waypoints/pinpoints on points of interest, attaching images and notes, and tracking routes, distance and elevation — all while offline.
“National Geographic has a century-long history of creating accurate, detailed maps used by travelers, explorers and map lovers across the globe. Today’s technologies allow us to continue that history in the digital realm, expanding the ways consumers can acquire and use our maps,” said Daniel Ortiz, vice president and general manager, National Geographic Maps. “As we celebrate 100 years of National Geographic mapmaking, we are excited to bring the popular Trails Illustrated map line to Avenza’s PDF Map app users.”
Avenza’s PDF Maps app provides constant access to geographic information and points of interest, with additional interactive tools such as measuring, place marking and location tagging. PDF Maps operates without the risk of lost reception due to cell tower proximity. It does not rely on an Internet connection.
“Avenza’s PDF Maps app provides the ability for anyone to share map-related information by documenting locations with customized notes, photos and descriptions,” said Ted Florence, president of Avenza Systems Inc. “This expands the utility of a map beyond location guidance, as it is also a tool to share experiences and locales. We continue to strengthen our community of map publishers while further advancing the mapping tools consumers demand, and we look forward to seeing how the industry evolves in an ever-mobile community.”
Avenza’s PDF Maps app is available now on the iTunes App Store and the Google Play Store, free of charge for personal use, with a Windows version coming soon. National Geographic maps can be accessed via the PDF Maps in-app store. Pricing of each map is set by the publisher, and free maps remain free to users through the PDF Maps app in-app store.
