Last glacial loess sedimentary system of eastern Nebraska and western Iowa

Places, topics & collections

Connections use shared source subjects, names, places, and explicitly mentioned entities. A shared label is not evidence of a citation, experimental result, or verified species identification.

Places & coverage

Source-reported bounding extents on a longitude/latitude grid. Boxes show coverage, not precise study locations.

• Last glacial loess sedimentary system of eastern Nebraska and western Iowa · 40.49709237269567° to 42.956422511073335° latitude, -99.42626953125° to -93.22998046875° longitude
• Statewide surficial geologic map of Nebraska underscores Quaternary landscape evolution from the High Plains to the Central Lowland · 39.999998° to 43.000585° latitude, -104.053249° to -95.30829° longitude
• Stability changes after weak layer collapse: Insights from an unexpected dataset · 45.3189460540203° to 45.33299318138492° latitude, -111.38445369182303° to -111.377294998524° longitude
• Tracking water in snow: Bridging sensor and and model simulations · 45.74021121503665° to 45.753680347339554° latitude, -110.92795556970783° to -110.89223903302934° longitude
• Patterns of glide avalanche release: Insights from 23 years of observations along the Going-to-the-Sun Road, Montana, USA · 48.61159695691762° to 48.824724984597566° latitude, -114.00684065662138° to -113.5122958000857° longitude
• Start-zone characteristics and timing of wet slab avalanches In Colorado · 36.97192343236556° to 40.982074695582696° latitude, -109.05376634727858° to -101.99984299334658° longitude
• Applying automated avalanche terrain mapping to wildlife ecology: A case study of Dall's sheep in southcentral Alaska · 60.933093530779416° to 62.4793223° latitude, -150.03156121483062° to -148.0393505° longitude
• Climate-driven shifts in snowpack conditions favorable for wet snow avalanches: Insights from snow cover model simulations · 48.16971779808773° to 49.0016388088892° latitude, -114.46808640264636° to -113.1760352579636° longitude
• Springs of the Catskill Mountains: A conduit flow system in predominantly siliciclastic strata · 41.883338180428126° to 42.33965461242107° latitude, -74.8435460287221° to -73.96130571248278° longitude
• Little Galloo Island, Lake Ontario: Two decades of studies on the diet, fish consumption, and management of double-crested cormorants · 43.88298525716862° to 43.88861453047109° latitude, -76.39892578125° to -76.39223098754883° longitude
• Paleomagnetic results from the Shasta Bally Plutonic Belt in the Klamath Mountains Province, northern California · 40° to 42° latitude, -123.25° to -121.75° longitude
• Comment on “Particle fluxes in groundwater change subsurface rock chemistry over geologic time” · 40.4323142901375° to 40.967455873296714° latitude, -78.17596435546875° to -77.33001708984375° longitude
• Estimating lake–climate responses from sparse data: An application to high elevation lakes · 36.94989178681327° to 41.04621681452063° latitude, -108.984375° to -104.4580078125° longitude
• Postbreeding movements and molting ecology of female gadwalls and mallards · 35.27972631361679° to 43.98744440673019° latitude, -122.76431186273942° to -117.71319968569426° longitude
• Shallow faulting and folding beneath south‐central Seattle, Washington State, from land‐based high‐resolution seismic‐reflection imaging · 47.4020813981619° to 47.62004863663242° latitude, -122.72997503110628° to -122.11956470840835° longitude
• Rainfall thresholds for postfire debris-flow initiation vary with short-duration rainfall climatology · 31.332239° to 42.009518° latitude, -124.409591° to -102.04224° longitude
• Beginner’s guide to understanding, accessing, and retrieving Coastwide Reference Monitoring System data · 28.71335539020771° to 30.391605679926187° latitude, -93.78247520861558° to -88.82426759799037° longitude
• Predicting Minnesota lake ice phenology with deep learning, explainable methods, and a physically based benchmark, 1980-2018 · 43.500415° to 49.383079° latitude, -97.239209° to -89.489226° longitude
• Water withdrawal and consumption trends for thermoelectric-power plants in the conterminous United States, 2008-2020 · 25.08° to 49.38905° latitude, -124.68721° to -66.96466° longitude
• New measurements indicate that natural geologic methane emissions from microseepage in the Michigan Basin are likely negligible · 42.865081723412004° to 46.54984228068227° latitude, -88.20025852293985° to -81.7815573772342° longitude
• Rearing method has limited effect on post-release movement of reintroduced age-0 Lake Sturgeon · 41.2309989857614° to 41.7578525° latitude, -84.27194190387294° to -82.1528812° longitude
• Age reassignment using luminescence dating for the Mammoth Site, Black Hills, South Dakota, USA · 43.412° to 43.437° latitude, -103.497° to -103.456° longitude
• The saline groundwater legacy of a large buried coastal paleo-estuary · 28.876181683683583° to 29.90397247495939° latitude, -92.18101678626572° to -89.03910819702195° longitude
• Lead exposure of snakes near recreational and military shooting areas in a sagebrush steppe ecosystem · 43.41589542240385° to 43.47177761405541° latitude, -116.45409722615386° to -116.37113818642081° longitude
• Northern bobwhites select for native grasses on working grazing land · 37.59201883997629° to 37.72406020069704° latitude, -84.3147403086961° to -84.10506369054549° longitude
• Long-term predictive modeling of stream condition suggests wide-spread changes within the Chesapeake Bay Watershed, USA · 36.658319982714204° to 42.6559974° latitude, -77.2729725° to -75.0820927° longitude
• Assessing the status and drivers of phytoplankton blooms along the riverine to freshwater-tidal continuum in a modified delta · 37.8001084° to 38.4927398° latitude, -121.9505123° to -121.3465035° longitude
• As above, so below? A framework for integrating long-term water quantity trends reveals divergent patterns in groundwater and low streamflow across the United States · 25.08° to 49.38905° latitude, -124.68721° to -66.96466° longitude
• Ecological transformations of coastal wetlands of the conterminous United States in response to contemporaneous sea-level rise · 25.08° to 49.38905° latitude, -124.68721° to -66.96466° longitude
• Testing characteristic magnitude distributions in modern PSHA models · 31.3159861° to 49.3838067° latitude, -125.7890305257902° to -102.7151136° longitude

Citation graph

Arrows run from the citing work to its reference. Only explicit source/provider reference lists are used. Incoming links cover this candidate window; this is not a global citation count.

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Collaborator network

Shared authorship within up to 200 candidate works (2 examined); up to 32 names shown. Names are matched as supplied, without verified person disambiguation. Shared credit does not necessarily establish personal collaboration.

Publication timeline

Publication years for these 32 related works; 0 have no source publication date. This is a discovery sample, not a measure of research output or growth.

Semantic map

Model: all-minilm. Positions are a two-dimensional approximation of embedding similarity; proximity is not a citation or proof of agreement. Results come from the snapshot’s candidate window.

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