Uranium in the Gas Hills area, Fremont and Natrona counties, Wyoming

1953 ◽  
Keyword(s):  

2000 ◽  
Author(s):  
Daniel G. Driscoll ◽  
Ghaith R. Hamade ◽  
Scott J. Kenner


2018 ◽  
Author(s):  
Shayna T. Avila ◽  
◽  
Jade Star Lackey ◽  
Brandon Lutz ◽  
Jeffrey R. Knott ◽  
...  


1963 ◽  
Vol 58 (2) ◽  
pp. 285-286 ◽  
Author(s):  
R. R. Guilinger
Keyword(s):  


2018 ◽  
Vol 25 (1) ◽  
pp. 1-14
Author(s):  
Acharya Balkrishna ◽  
◽  
Anupam Srivastava ◽  
B.K. Shukla ◽  
Rajesh Kumar Mishra ◽  
...  

During plant exploration and survey of Morni Hills, Panchkula, Haryana (2017-2018) the authors collected about 2200 field numbers from different localities. Out of them, 323 species belonging to 251 genera and 92 families are medicinal plants. The information about medicinal properties of these plants has been gathered during field trips of Morni Hills from local vaidyas and local people of remote localities. The enumeration is alphabetically arranged, followed by their family names, local/common names, plant parts used for curing diseases and medicinal uses. These plant species are utilized by local people against various diseases in Morni Hills area.



Author(s):  
Puput Dani Prasetyo Adi ◽  
Fransiska Sisilia Mukti ◽  
Panggih Nur Adi ◽  
Akio Kitagawa ◽  
Toni ◽  
...  
Keyword(s):  


Geophysics ◽  
2000 ◽  
Vol 65 (5) ◽  
pp. 1514-1526 ◽  
Author(s):  
Alvin K. Benson ◽  
Andrew R. Floyd

Gravity and magnetic data were collected in the Mosida Hills, Utah County, Utah, at over 1100 stations covering an area of approximately 58 km2 (150 mi2) in order to help define the subsurface geology and assess potential geological hazards for urban planning in an area where the population is rapidly increasing. In addition, potential hydrocarbon traps and mineral ore bodies may be associated with some of the interpreted subsurface structures. Standard processing techniques were applied to the data to remove known variations unrelated to the geology of the area. The residual data were used to generate gravity and magnetic contour maps, isometric projections, profiles, and subsurface models. Ambiguities in the geological models were reduced by (1) incorporating data from previous geophysical surveys, surface mapping, and aeromagnetic data, (2) integrating the gravity and magnetic data from our survey, and (3) correlating the modeled cross sections. Gravity highs and coincident magnetic highs delineate mafic lava flows, gravity lows and magnetic highs reflect tuffs, and gravity highs and magnetic lows spatially correlate with carbonates. These correlations help identify the subsurface geology and lead to new insights about the formation of the associated valleys. At least eight new faults (or fault segments) were identified from the gravity data, whereas the magnetic data indicate the existence of at least three concealed and/or poorly exposed igneous bodies, as well as a large ash‐flow tuff. The presence of low‐angle faults suggests that folding or downwarping, in addition to faulting, played a role in the formation of the valleys in the Mosida Hills area. The interpreted location and nature of concealed faults and volcanic flows in the Mosida Hills area are being used by policy makers to help develop mitigation procedures to protect life and property.





Sign in / Sign up

Export Citation Format

Share Document