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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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Egypt
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Kharga Oasis (1)
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Morocco
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Moroccan Atlas Mountains
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High Atlas (1)
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Atlantic Ocean Islands
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Canary Islands
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Gomera (1)
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Europe
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Southern Europe
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Italy
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Calabria Italy
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Sila Massif (1)
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Green River (1)
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Sierra Nevada (1)
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Table Mountain (1)
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United States
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California
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Tuolumne County California (1)
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Utah
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Emery County Utah (1)
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Western Desert (1)
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elements, isotopes
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isotopes
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radioactive isotopes
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Be-10 (1)
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metals
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alkali metals
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potassium (1)
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alkaline earth metals
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beryllium
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Be-10 (1)
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geochronology methods
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(U-Th)/He (1)
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fission-track dating (1)
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K/Ar (1)
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paleomagnetism (1)
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thermochronology (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene (1)
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Tertiary
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Neogene
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Miocene (1)
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Pliocene (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Cedar Mountain Formation (1)
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Jurassic
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Upper Jurassic
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Brushy Basin Member (1)
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Morrison Formation (1)
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Salt Wash Sandstone Member (1)
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Paleozoic (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts (1)
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latite (1)
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Primary terms
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absolute age (2)
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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-
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Egypt
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Kharga Oasis (1)
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Morocco
-
Moroccan Atlas Mountains
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High Atlas (1)
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-
-
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Atlantic Ocean Islands
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Canary Islands
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Gomera (1)
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Cenozoic
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Quaternary
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Holocene (1)
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Tertiary
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Neogene
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Miocene (1)
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Pliocene (1)
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diagenesis (1)
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Europe
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Southern Europe
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Italy
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Calabria Italy
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Sila Massif (1)
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faults (1)
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folds (1)
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geochronology (1)
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geomorphology (2)
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igneous rocks
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volcanic rocks
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basalts (1)
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latite (1)
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isotopes
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radioactive isotopes
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Be-10 (1)
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mantle (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Cedar Mountain Formation (1)
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Jurassic
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Upper Jurassic
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Brushy Basin Member (1)
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Morrison Formation (1)
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Salt Wash Sandstone Member (1)
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metals
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alkali metals
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potassium (1)
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alkaline earth metals
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beryllium
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Be-10 (1)
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Moon (1)
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orogeny (1)
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paleoclimatology (1)
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paleomagnetism (1)
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Paleozoic (1)
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plate tectonics (1)
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tectonics (1)
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United States
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California
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Tuolumne County California (1)
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Utah
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Emery County Utah (1)
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relief inversion
Evaluating the role of topographic inversion in the formation of the Stanislaus Table Mountains in the Sierra Nevada (California, USA)
Deriving rock uplift histories from data-driven inversion of river profiles
Field guide to exhumed paleochannels near Green River, Utah: Terrestrial analogs for sinuous ridges on Mars
Multiple cemented channel-fill deposits from the Late Jurassic and Early Cretaceous, once buried beneath 2400 m of sediment, are now exposed at the surface in arid east-central Utah due to erosion of the less resistant surrounding material. This field guide focuses on examples near the town of Green River where there is public access to several different types of exhumed paleochannels within a small geographic region. We describe the geologic setting of these landforms based on previous work, discuss the relevance to analogous sinuous ridges that are interpreted to be inverted paleochannels on Mars, and present a detailed road log with descriptive stops in Emery County, Utah.
The Gruithuisen region in northern Oceanus Procellarum on the Moon contains three distinctive domes interpreted as nonmare volcanic features of Imbrian age. A 4 d extravehicular activity (EVA), four-astronaut sortie mission to explore these enigmatic features and the surrounding terrain provides the opportunity to address key outstanding lunar science questions. The landing site is on the mare south of Gruithuisen 3 (36.22°N, 40.60°W). From this site, diverse geologic terrains and features are accessible, including highlands, dome material, mare basalts, multiple craters, small rilles, and a negative topographic feature of unknown origin. Preliminary mission planning is based on Clementine multispectral data, Lunar Prospector geochemical estimates, and high-resolution (0.5 m/pixel) stereo images from the Lunar Reconnaissance Orbiter Narrow Angle Camera. Science objectives for the mission include: (1) determining the nature of the domes, (2) identifying and measuring the distribution of any potassium, rare earth elements, and phosphorus (KREEP)- and thorium-rich materials, (3) collecting samples for age dating of key units to investigate the evolution of the region, and (4) deploying a passive seismic grid as part of a global lunar network. Satisfying the science objectives requires 7 h, ~20 km round-trip EVAs, and significant time driving on slopes up to ~15°.