“Snake river Overlook” landslide, Apr. 28th, 2005

The Yellowstone-snake River Plain Seismic Profiling Experiment: Crustal Structure of the Eastern Snake River Plain

Seismic refraction profiles recorded layer. Crustal subsidence and periodic basaltic along the eastern Snake River Plain (ESRP) in southeastern Idaho during the 1978 YellowstoneSnake River Plain cooperative seismic profiling experiment are interpreted to infer the crustal velocity and attenuation (Q-i) structure of the ESRP. Travel-time and synthetic seismogram modeling of a 250 km reversed ref...

Landslide erosion coupled to tectonics and river incision

The steep topography of mountain landscapes arises from interactions among tectonic rock uplift, valley incision and landslide erosion on hillslopes. Hillslopes in rapidly uplifting landscapes are thought to respond to river incision into bedrock by steepening to a maximum stable or ‘threshold’ angle1–3. Landslide erosion rates are predicted to increase nonlinearly as hillslope angles approach ...

Screening programs overlook transgender people.

Non-Native (Exotic) Snake Envenomations in the U.S., 2005–2011

Non-native (exotic) snakes are a problematic source of envenomation worldwide. This manuscript describes the current demographics, outcomes and challenges of non-native snakebites in the United States (U.S.). We performed a retrospective case series of the National Poison Data System (NPDS) database between 2005 and 2011. There were 258 human exposures involving at least 61 unique exotic venomo...

Effects of Flow Augmentation on Snake River Fall Chinook

Table 6. Flow survival regression S = a + b * Flow for seasonal data average by unweighted and weighted by smolt passage index. ∆S = (S 80-S 70)/ S 80 is a relative increase in survival with a 10 kcfs increase in flow where S 80 and S 70 are survivals at 80 and 70 kcfs Lower Table 15a. Scenario average flows (kcfs) and temperatures (centigrade) plus flow augmentation (maf) between day 160 and 2...