3,823 research outputs found

    Soil information sheets for the northern agricultural areas

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    These soil information sheets are produced for farmers in the Northern Wheatbelt. Each sheet summaries information on the particular soil\u27s characteristic properties and associated land use suitability and management. A photograph of a representative profile is provided for each soil. Technical terms are defined in the glossary. Information is presented under the following headings: Soil series and group, occurrence, native vegetation, soil profile description, characteristic soil properties, soil classification (Australian Soil Classification and Northcote Principal Profile Form)

    Keeping Your Home: A Guide to Foreclosure Prevention and Assistance in Prince George's County, MD

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    Offers step-by-step guidance on avoiding foreclosure and negotiating with lenders. Explains foreclosure and eviction procedures. Includes lists of housing counseling agencies, emergency service organizations, and government programs

    CPA expert 2000 fall/winter 2001

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    https://egrove.olemiss.edu/aicpa_news/1042/thumbnail.jp

    Spokane Intercollegiate Research Conference 2014

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    Local Government Law

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    Exhibiting and judging garden vegetables (2012)

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    Whether on an individual basis at fairs or in 4-H, FFA or a garden club competition, exhibiting vegetables is an excellent way to learn more about quality and handling of vegetables. While setting up an exhibit, you have a chance to meet others with similar interests and learn from them. Win or lose, you can learn from the experience and accept the challenge to improve future displays and exhibits.Reviewed 1/12/2M

    Human Response to Late Holocene Climate Change at the Patrick Site (40MR40) in East Tennessee

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    Current archaeological research links Late Holocene climate variability to patterns of dispersal and reorganization during the Archaic-Woodland transition in the Southeast (3200-2400 cal BP). This study uses geomorphic and archaeological proxy data from curated soil monoliths collected at the Patrick site (40MR40), located in Monroe County along the Little Tennessee River in Tennessee, to the assess the impact of Late Holocene climate change on the Late Archaic and Early Woodland groups that utilized the river valley. The results of these analyses indicate that the progressive downcutting of the river, apparent in sediments dating between 5700-3600 cal BP, had an ameliorating effect on the floodplain landscape that preceded the intensified use of first river terrace during the Terminal Late Archaic Iddins phase and Early Woodland Watts Bar phase.Decreases in coarse grain sediments associated with high-energy flooding and subsequent increases in cumulic soil formation at the Patrick site demonstrate that the floodplain environment had begun to stabilized during the Late Archaic period at approximately 3600 cal BP. This pattern is followed by dense midden accumulation, increases in the occurrence of cultivated plant foods, and a precipitous increase in pottery associated with Early Woodland Watts Bar and Patrick phase occupations at the site; suggesting that local populations took advantage the increasingly inhabitable floodplain environment. This study posits that the relatively cooler and wetter climate conditions of the Late Holocene Subboreal climate period (5000-2400 cal BP) may not have had a disruptive effect on prehistoric populations in the lower Little Tennessee River valley, contrasting what has been observed elsewhere in the Southeast during the Archaic-Woodland transition

    Observations of the geology and geomorphology of the 1999 Marsokhod test site

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    The Marsokhod rover returned data from six stations that were used to decipher the geomorphology and geology of a region not previously visited by members of the geomorphology field team. Satellite images and simulated descent images provided information about the regional setting. The landing zone was on an alluvial apron flanking a mountain block to the west and playa surface to the east. Rover color images, infrared spectra analysis of the mountains, and the apron surface provided insight into the rock composition of the nearby mountains. From the return data the geomorphology team interpreted the region to consist of compressionally deformed, ancient marine sediments and igneous rocks exposed by more recent extensional tectonics. Unconsolidated alluvial materials blanket the lower flanks of the mountains. An ancient shoreline cut into alluvial material marks a high stand of water during a past, wetter climate period. Playa sediments floor a present-day, seasonally, dry lake. Observations made by the rover using panoramic and close-up (hand specimens—scale) image data and color scene data confirmed the presence of boulders, cobbles, and fines of various provinces. Rover traverses to sites identified as geologically distinct, such as a fan, channel, shoreline, and playa, provided useful clues to the geologic interpretations. Analysis of local rocks was given context only through comparison with distant geologic features. These results demonstrated the importance of a multifaceted approach to site interpretation through comparison of interpretations derived by differing geologic techniques
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