This 1:50,000 scale geologic map describes the distribution of unconsolidated deposits, identifies local geologic hazards, and provides information about the depositional environment and basic engineering properties of common surficial-geologic materials in and around Shaktoolik, Alaska. Map units are the result of combined field observations and aerial imagery interpretation. A suite of local ground observations were collected over a two-week period in July 2011 by a helicopter-supported team of DGGS geologists and collaborators. Field investigations included soil test pits, sample collection, soil and rock description, oblique aerial photography, and documentation of landscape morphology.

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URL: https://geoscience.data.qld.gov.au/dataset/mr006368

The NORTON Mine map was published at 4 Chains to an Inch as part of the TOWN MAP series to administer permit and permit related spatial information. The map was maintained internally as a provisional office chart and is located within the Calliope (9149) 1:100 000 map area.
The map product is available to all government agencies, industry and the public for reference.
Title and Image reference number is NORTON_2558.

Cancelled 1982

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URL: https://geoscience.data.qld.gov.au/dataset/cr055364

GSQ PUBLICATION 208, REPORT ON THE NORTON GOLDFIELD (WITH ONE MAP AND FOUR PLATES)

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Restaurants in Norton, Massachusetts. name, maps, price Range, types, city, continent, Country, Website, email, administrative división, address, telephone

Layered GeoPDF Quadrangle Map. Layers of geospatial data include orthoimagery, roads, grids, geographic names, elevation contours, hydrography, and other selected map features.

U.S. Census Bureau QuickFacts statistics for Norton Shores city, Michigan. QuickFacts data are derived from: Population Estimates, American Community Survey, Census of Population and Housing, Current Population Survey, Small Area Health Insurance Estimates, Small Area Income and Poverty Estimates, State and County Housing Unit Estimates, County Business Patterns, Nonemployer Statistics, Economic Census, Survey of Business Owners, Building Permits.

The period 1691 to 1729 was a time of relative inactivity for exploration in areas of concern to New France and England. The main journeys were out of Louisiana to explore the Mississippi and its tributaries, and, much further north, there were some forays into Hudson Bay conducted or ordered by Henry Kelsey of the Hudson's Bay Company. Nine explorer routes are shown: Le Sueur (1700 to 1701), Bourgmont (1714), Kelsey (1690 to 1692), Stuart (1715 to 1716), De Vincennes (1696 to 1704), Louis Jolliet (1694), De Courtemanche (1704), Kelsey (1719) and Scroggs and Norton (1722). The map also shows the extent of territory known to Europeans and the navigation of all exploration routes in the period 1651 to 1760. The historical names found on the map are derived from contemporaneous maps and written documents of the period.

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Bedrock geologic map of the Big Hurrah-Council-Bluff area, Southern Seward Peninsula, Alaska, Report of Investigation 2024-7, presents bedrock geologic mapping from the blueschist-facies-metamorphosed, Late Proterozoic to Devonian Nome Complex was conducted by the Alaska Division of Geological & Geophysical Surveys (DGGS) on southern Seward Peninsula, Alaska. This map, covering portions of the Solomon C-4, C-5, D-4, D-5, and the southern Bendeleben A-4 quadrangles, includes new mapping by DGGS in the summer of 2006 and incorporates previous mapping conducted by DGGS in 2003 and 2004. Surficial geologic mapping was also conducted in the area. This 595-square-mile, 1:50,000-scale, bedrock geologic map coincides with portions of the DGGS Council airborne magnetic and resistivity survey. The geophysical survey and geologic map are part of the State of Alaska's Airborne Geophysical/Geological Mineral Inventory program, focusing on enhancing public knowledge of Alaska's geology and mineral districts. More than 1 million ounces of placer gold have been extracted from the map area since the turn of the century, with most production derived from the Casadepaga and Solomon rivers and Ophir Creek. Widespread low-sulfide, gold-bearing quartz veins of Cretaceous age were the primary lode source for the placer gold. Approximately 27,000 ounces of gold were produced from low-sulfide quartz veins at the Big Hurrah lode gold mine between 1903 and 1907. Other notable lode gold prospects in the map area include Silver (Flynn), West Creek, and an unnamed prospect at the head of Albion Creek. The Bluff area along Norton Sound has both lode gold and mercury prospects. The map area contains numerous occurrences of silicified marble with anomalous geochemistry of uncertain age and genetic origin. Various lithologies of the Layered sequence subdivision of the Nome Complex, primarily the Mixed unit, have the potential to host sedimentary exhalative (SEDEX) mineralization of Late Devonian to possibly Mississippian(?) age, as found elsewhere on the Seward Peninsula. The complete report, geodatabase, and ESRI fonts and style files are available from the Alaska Division of Geological & Geophysical Surveys website: http://doi.org/10.14509/31308.

Credit report of Meghan Norton contains unique and detailed export import market intelligence with it's phone, email, Linkedin and details of each import and export shipment like product, quantity, price, buyer, supplier names, country and date of shipment.

The current threats of climate change have prompted the dependency on groundwater as a sustainable supply of domestic water. As a result, maintaining groundwater quality has remained a critical intervention for many local authorities especially in developing countries including Zimbabwe. This study assessed the vulnerability of groundwater quality within Norton Townin Zimbabwe, an urban area that dependents partly on groundwater sources for domestic water supplies.The town has a number of potential pollution sources. Potential pollution sources were digitized onGoogleEarth mapusing GIS techniques. Ground control points were collected to validate and improve the potential pollution source map. Fifteen (15) systematically selected groundwater points (8 boreholes and 7 wells) located close to potential pollution sources were chosen and water samples collected from them. Four (4) sampling campaigns were undertaken in January and February 2016. The water samples were analysed for selected water quality parameters using standard methods and compared to Zimbabwean and World Health Organization limits to assess drinking suitability. The parameters that were studied include temperature, turbidity, pH, DO, electrical conductivity, TDS, total hardness, iron, sulphates, chlorides, faecal coliform and total coliform. One-way Analysis of Variance was performed using SPSS version 23 to test for any significant differences between parameters and sites. In order to determine parameters that are important in assessing variation in groundwater quality data set, Principal Component Analysis was used. The Moving Average technique in Integrated Land and Water Information System was used to plotspatial and temporal variation of groundwater in the environment. The Aquifer Vulnerability Index Model was used for mapping the vulnerability of groundwater in Norton Town. Six parameters including hydraulic conductivity, soil media, depth to water level, aquifer media, slope and land cover were assigned weights and ratings using ILWIS Software. Statistical data grouping was implemented in order to differentiate five categorical index ranges.Results for mapping potential pollution sources showedthat, industrial activities and improper disposal of solid wastes and wastewater are the main causes of groundwater pollution in Norton. Descriptive statistics for the analysed groundwater parameters showed the mean values for temperature, turbidity, pH, DO, electrical conductivity, TDS, total hardness, iron, sulphates, chlorides, faecal coliform and total coliform were 25.7 °C, 6.8 NTU, 7.2, 3.66 mg/L, 580 μS/cm, 280 mg/L, 698 mg/L, 0.05 mg/L, 455 mg/L, 282 mg/L, 1015 cfu/100mL, 991 cfu/100mLrespectively. The resultsshowed that temperature, turbidity, DO, TDS, pH, chlorides, total hardness, electrical conductivity and sulphates had significant variation of parameters (spatial and temporal) explained by (p values <0.05). PCA components F1, F2, F3 and F4 had total variability of 80% with each one of the components having 36%, 24%, 11% and 9% respectively.The significant parameterswerechlorides, dissolved oxygen, electrical conductivity and feacal coliform. From the Aquifer Vulnerability IndexModel, five different vulnerability zones were established which were; very low vulnerability (index 63-73), low vulnerability (74-84), moderate vulnerability (85-95), high vulnerability (95-106) and very high vulnerability (107-126). The results showed that 17.8% of the area had very low vulnerability, 37.2% low vulnerability, 30% moderate vulnerability, 12.5% high vulnerability and 2.5% very high vulnerability. The study identified the main pollution sources as treatment plant, agriculture, landfill, onsite sanitation and industrial discharge. The study also revealed that potential pollution sources are the main causes of groundwater contamination. The results showed that groundwater sources situated in high density areas had faecal coliform counts greater than 100 cfu/100 mL which could be harmful to human health. Groundwater quality parameters (50 %) exceeded the Zimbabwean and World Health Organisation drinking water limits. At the present moment, the area shows a total of55 % very low to low vulnerability.It is therefore recommended that water from vulnerable sources be disinfected regularly before human consumption. WaterNet

Restaurantes en Norton, Ohio. nombre, maps, rango de precios, tipos, ciudad, continente, País, Sitio web, email, división administrativa, dirección, teléfono

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