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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Simultaneous Middle Pleistocene eruption of three widespread tholeiitic basalts in northern California (USA): Insights into crustal magma transport in an actively extending back arc Available to Purchase
The remarkable volcanism of Shastina, a stratocone segment of Mount Shasta, California Open Access
The timing and compositional evolution of volcanism within northern Harrat Rahat, Kingdom of Saudi Arabia Available to Purchase
Eruption age and duration of the ∼9 km 3 Burney Mountain dacite dome complex, northern California, USA Available to Purchase
Volcanic stratigraphy and age model of the Kimama deep borehole (Project Hotspot): Evidence for 5.8 million years of continuous basalt volcanism, central Snake River Plain, Idaho Open Access
Volcanic history of the northernmost part of the Harrat Rahat volcanic field, Saudi Arabia Open Access
Holocene volcanism of the upper McKenzie River catchment, central Oregon Cascades, USA Open Access
Holocene volcanism of the upper McKenzie River catchment, central Oregon Cascades, USA Available to Purchase
Geochemical and paleomagnetic variations in basalts from the Wendell Regional Aquifer Systems Analysis (RASA) drill core: Evidence for magma recharge and assimilation–fractional crystallization from the central Snake River Plain, Idaho Open Access
Owyhee River intracanyon lava flows: Does the river give a dam? Available to Purchase
Kulanaokuaiki Tephra (ca. A.D. 400–1000): Newly recognized evidence for highly explosive eruptions at Kīlauea Volcano, Hawai‘i Available to Purchase
The post-Mazama northwest rift zone eruption at Newberry Volcano, Oregon Available to Purchase
Abstract The northwest rift zone (NWRZ) eruption took place at Newberry Volcano ~7000 years ago after the volcano was mantled by tephra from the catastrophic eruption that destroyed Mount Mazama and produced the Crater Lake caldera. The NWRZ eruption produced multiple lava flows from a variety of vents including cinder cones, spatter vents, and fissures, possibly in more than one episode. Eruptive behaviors ranged from energetic Strombolian, which produced significant tephra plumes, to low-energy Hawaiian-style. This paper summarizes and in part reinterprets what is known about the eruption and presents information from new and ongoing studies. Total distance spanned by the eruption is 32 km north-south. The northernmost flow of the NWRZ blocked the Deschutes River upstream from the city of Bend, Oregon, and changed the course of the river. Renewed mafic activity in the region, particularly eruptions such as the NWRZ with tephra plumes and multiple lava flows from many vents, would have significant impacts for the residents of Bend and other central Oregon communities.
Revised ages for tuffs of the Yellowstone Plateau volcanic field: Assignment of the Huckleberry Ridge Tuff to a new geomagnetic polarity event Available to Purchase
Paleoenvironments of sedimentary interbeds in the Pliocene and Quaternary Big Lost Trough, eastern Snake River Plain, Idaho Available to Purchase
Full article available in PDF version.
Tension cracks, eruptive fissures, dikes, and faults related to late Pleistocene-Holocene basaltic volcanism and implications for the distribution of hydraulic conductivity in the eastern Snake River Plain, Idaho Available to Purchase
Full article available in PDF version.
Accumulation and subsidence of the Pleistocene basaltic lava flows of the eastern Snake River Plain, Idaho Available to Purchase
Full article available in PDF version.