Calling all photographers! NBMG is already accepting photographs for the Nevada Geology Calendar 2016. If you have photographs of interesting geologic features or landscapes from your fieldwork that you would like to submit for next year’s calendar, please email Jack Hursh at NBMG.
Here are the details for this contest for the 2016 calendar:
- Deadline for entries isMay 31, 2015
- Photos need to be taken in Nevada. A location description and/or GPS coordinates should accompany submissions along with description.
- High-quality, high-resolution photo files of at least 300 dpi are required for quality printing.
- E-mail submissions to Jack Hursh (firstname.lastname@example.org).
- NBMG cartographers will make the final decision on the winning photos.
- Prizes will be awarded for first-, second-, and third-place winners.
Congratulations to the winners of the Nevada Geology Calendar 2015 photo contest!
First-place winner: Gregg Beukelman
February photo of “Cathedral Gorge State Park, Lincoln County”
Second-place winner: Chip Carroon
September photo of “Outcrops of Precambrian gneiss at Overland Lake in the Ruby Mountains, Elko County”
Third-place winner: Angel LaCanfora
Rock Types page photo of “Aztec Sandstone, Fire Canyon, Valley of Fire State Park, Clark County”
Fourth-place winner (bonus prize): Bryan Norman
October photo of “Cambrian quartzite on Wheeler Peak and Stella Lake, White Pine County”
Thank you all for your wonderful photo contributions! First-, second-, and third-place winners will receive a copy of the calendar and a business card holder made from rhyolite vitric tuff with black pumice fragments of Tertiary age from Jackpot, Elko County. Fourth-place winner will receive a calendar and lapel pin. We would like to thank Jon Price for making and donating these beautiful business card holders and pin.
Click here for printable PDF of this advertisement.
Nevada Geology Calendar 2015, designed by Jack Hursh, Jennifer Vlcan, Chris Henry, and Nick Hinz, 2014
This 12-month calendar (January 2015 through December 2015) features a different geologic topic each month: Snow Covered, Lacustrine Sediments, Pahranagat Shear Zone, Sandstone, Natural Arches, Hot Springs, Las Vegas Valley, Metamorphic Rocks, Ruby Mountains, High Alpine, Folded Rock, Black Rock Desert, and Abandoned Mine Safety. It is full of beautiful photos highlighting Nevada’s scenic wonders and also includes interesting facts about Nevada geology that really make you want to go and visit those sites.
13 x 9.5 inches, $15.00
Here are the available discounts for the public:
5-10 calendars (10% discount), $13.50 each
10+ calendars (20% discount), $12.00 each
These would make wonderful holiday gifts for your friends or clients.
Please note: If you place an order for 5 or more calendars, the shopping cart will complete your order showing the regular price. That is OK. When we process the order, we will reduce your total to reflect the discounted price before we submit the charge to VeriSign/PayPal. You will only be charged the discounted amount, and that discounted amount will be on your receipt that we send with your package.
Click here to order: http://www.nbmg.unr.edu/sales/pbsdtls.php?sku=CAL2015
You may also call us at 775-682-8766 to place an order.
For those on the UNR campus who would like free delivery, you may select “Pick up” on the shopping cart so you will not be charged for shipping and then under “instructions” type “UNR campus mail delivery.” Please be sure to give us your campus mail stop and department name.
Walk-in purchase: Calendars are also available for sale at the Great Basin Science Sample and Records Library (2175 Raggio Parkway, Reno).
We will be closed November 27-28 for Thanksgiving.
A big thank you goes to Jack Hursh, Jennifer Vlcan, Chris Henry, and Nick Hinz for creating another beautiful calendar this year!
NBMG T-shirts are now back in stock, and here’s the scoop:
- They are available in sizes for ladies and men (colors and sizes listed below).
- All shirts are $18.00.
- The front of the T-shirts has an “N” logo for “University of Nevada” and also the NBMG logo and name.
- The back of the shirt has a simplified version of the NBMG Geologic Map of Nevada.
You need to call 775-682-8766 to place an order for a T-shirt. The shirts are not currently available on the shopping cart but will be added in about a month.
Click here to view the men’s shirts: http://www.nbmg.unr.edu/_docs/T-shirts_mens.pdf
Click here to view the ladies’ shirts: http://www.nbmg.unr.edu/_docs/T-shirts_ladies.pdf
For those on the University of Nevada, Reno campus who would like free delivery, please let us know when you call to place an order.
A note from Stacia Gordon, Geological Sciences & Engineering: We will have two short (about 30 minutes each) talks today as part of our seminar series:
1) Sergey A. Konyshev, UNR MS Student
Geochemistry and Petrography of the Beartrack Mine property, Lemhi County, Idaho
2) Mike Ressel, new NBMG faculty
The Golden Years: Eocene Metallogeny in the Silver State
See you all there: University of Nevada, Reno campus; DMS 105, 4-5 pm, followed by the social hour in LME 322D
Open-File Report 14-6
Preliminary geologic map of Heath Canyon, central Grant Range, Nye County, Nevada, by Sean P. Long, 2014
New 1:24,000-scale mapping across the full width of the central Grant Range, in a transect-style map located east of the Grant Canyon and Bacon Flat oil fields in Railroad Valley, provides valuable context for relating the structural style and geometry within the range to the subsurface structure of the oil fields. Sedimentary rocks between Cambrian and Pennsylvanian in age, and Eocene to Oligocene sedimentary and volcanic rocks, are exposed in the map area. Cambrian and Ordovician rocks have been metamorphosed to greenschist facies and experienced penetrative ductile deformation, likely during the Cretaceous. Two separate sets of normal faults deform the section, including an older set of down-to-the-west detachment faults that eliminate stratigraphy, and formed at low angles to bedding, and a younger set of high-angle, cross-cutting normal faults, including a range-bounding fault with multiple Holocene surface ruptures. Several detachment faults cut Oligocene volcanic rocks, providing a maximum age bound for the older episode of extension.
This publication was prepared as part of the STATEMAP component of the National Cooperative Geologic Mapping Program in cooperation with the U.S. Geological Survey.
Open-File Report 14-6, scale 1:24,000, 41 x 26 inches, color; 4-page text, b/w; folded or rolled, $16.00 for paper copy–or free on the Web:
Open-File Report 13-10 (second edition)
Preliminary geologic map of the central Lake Range, southern Fox Range, and northern Terraced Hills, Emerson Pass geothermal area, Washoe County, Nevada, by Ryan B. Anderson, James E. Faulds, and Gregory M. Dering, 2014
Detailed geologic mapping and stratigraphic-structural analyses have elucidated the kinematics, stress state, and structural controls of a “blind” geothermal system in Emerson Pass on the Pyramid Lake Paiute Tribe Reservation, western Nevada. The Emerson Pass area resides near the boundary of the Basin and Range and Walker Lane provinces of northwestern Nevada, at the northeast end of Pyramid Lake. Strata of the surrounding Fox Range, Lake Range, and Terraced Hills are comprised of late Miocene to Pliocene sedimentary rocks and the middle Miocene Pyramid sequence volcanic rocks, all overlying Cretaceous intrusions and Triassic to Jurassic metasedimentary rocks.
The active geothermal system is expressed as a 2-m shallow temperature thermal anomaly (maximum ∼60°C) that lies at the western edge of a broad left step at the northeast end of Pyramid Lake between the north- to north-northeast-striking, west-dipping, Fox and Lake Range normal faults. The 2-m temperature surveys have defined a north-south elongate thermal anomaly that resides on a north- to north-northeast-striking normal fault. Additionally, travertine mounds, chalcedonic silica veins, and silica-cemented Pleistocene lacustrine gravels in Emerson Pass indicate a robust geothermal system active at the surface in the recent past, likely the early Holocene. Structural complexity and spatial heterogeneities of the strain and stress field have developed in the step-over region, but kinematic data suggest a west-northwest-trending (∼280° azimuth) extension direction. The geothermal system is likely hosted in Emerson Pass as a result of enhanced permeability generated by the intersection of two oppositely dipping, southward- terminating north- to north-northwest-striking (Fox Range fault) and north-northeast-striking normal faults.
This publication was prepared with support from the U.S. Department of Energy. We thank the Pyramid Lake Paiute Reservation for access to tribal lands and logistical support throughout the project.
Geochronologic data (several 40Ar/39Ar dates) were added to this second edition.
Open-File Report 13-10 (second edition, 2014) supersedes the first edition (2013).
Open-File Report 13-10 (second edition), one color plate with 3 cross sections, 51.5 x 39.5 inches, scale 1:24,000; inset map, scale 1:8,000; 10-page text, b/w, $22.00 for paper copy—or free on the Web: