The ecological impact of conquest and colonization on a medieval frontier landscape: combined palynological and geochemical analysis of lake sediments from Radzyń Chełminski, northern Poland

Slavic and German colonization of the southern Baltic between the 8th and 15th centuries A.D. is well-documented archaeologically and historically. Despite the large number of pollen profiles from Poland, few palaeoecological studies have examined the ecological impact of a process that was central to the expansion of European, Christian, societies. This study aims to redress this balance through multiproxy analysis of lake sediments from Radzyń Chełminski, Northern Poland, using pollen, element geochemistry (Inductively Coupled-Optical Emission Spectroscopy [ICP-OES]), organic content, and magnetic susceptibility. The close association between lake and medieval settlements presents the ideal opportunity to reconstruct past vegetation and land-use dynamics within a well-documented archaeological, historical, and cultural context. Three broad phases of increasing landscape impact are visible in the pollen and geochemical data dating from the 8th/9th, 10th/11th, and 13th centuries, reflecting successive phases of Slavic and German colonization. This involved the progressive clearance of oak-hornbeam dominated woodland and the development of an increasingly open agricultural landscape. Although the castles and towns of the Teutonic Order remain the most visible signs of medieval colonization, the palynological and geochemical data demonstrate that the major phase of woodland impact occurred during the preceding phase of Slavic expansion; Germans colonists were entering a landscape already significantly altered.

The Impact of Land Use Patterns and Watershed Characteristics on China Lake, Kennebec County, Maine

China Lake is located in Kennebec County, Maine. Since 1983 the lake has suffered from yearly algal blooms as a result of the addition of excess nutrients. The nutrient load was amplified by erosion within the watershed. Erosion varies widely depending on a number of factors, including the slope of the land, the type of soil, and the way the land is being used. Certain land use types have a high potential to add nutrients to the environment, while others may help absorb excess nutrients and prevent erosion and runoff into the lake. A comprehensive examination of the China Lake watershed was completed using GIS to calculate the erosion potential for the entire area, taking into account past and present land use patterns. This information will help the towns around the lake to make informed decisions about future development and land management.

Reinstating indigenous landscape planning curatorship : the Lake Condah restoration project

While contemporary Western planning traditions in Australia talk of the last 200 years of innovation and transposition of European and North American planning traditions upon the Australian landscape, they neglect to mention some 40-50,000 years of Indigenous landscape planning initiatives and practice. The ancestral country of the Gunditjmara people is in the Western District of Victoria focused upon the Lake Condah and Mount Eccles localities. The Gunditjmara had, and continue to have a strong social, cultural and land management and planning presence in the region, in particular linked to environmental engineering initiatives and aquaculture curatorship of eel and fish resources. Archaeological evidence confirms that some 10,000 years of pre-European contact landscape planning practice has been applied by the Gunditjmara to construct resources management infrastructure to service a regional food need as well as a community need. Within contemporary reconciliation discourses, the Gunditjmara have activity sought over the last 25 years the rehabilitation of Lake Condah, which is now coming into fruition, and the restoration of their traditional landscape planning and management responsibilities. This paper reviews the restoration of Indigenous landscape planning and management theory and practice by the Gunditjmara, pointing to significant policy and practice success as well as the need to better appreciate this culturally-attuned and ecologically-responsive approach to landscape planning borne out of generations of knowledge.

Learning from sustainable landscapes of death in Bali : landscape planning and Tri Hita Karana

Landscape planning in many countries is predicated upon on fulfilling the functions for human living objectives. Many land use practices have been plotted for living, busines~, trading, industrial, farming as well as providing places for dead people primarily through cemeteries. Research in Palm Beach County, FL, has demonstrated the need to plan for 30 years of demand of land use functions to service death (Coutts, Basmaj ian et al. 20 I I). Coutts et al assert that planners are required and responsible for the planning of funeral necessities. Therefore, the protection of landscapes of death is an important consideration in the planning of landscapes. Bali is popular with its beautiful landscape, hospitality, and traditional architecture as demonstrating the integrity between human, environment and God, as expressed in the Balinese Tri Hita Karana concept. Balinese commemorate life from birth to death through their traditional ceremonies which informs their traditional cultural landscape. One of the most important landscapes, which cannot be separated fi·om Balinese life are graveyards which are used for deceased ceremonies. This landscape is an integral part of traditional village patterns across Bali. Culturally, Balinese people have their own traditional cremation ceremony which is call the Ngaben Ceremony. The Ceremony takes place in graveyards and thereupon ashes are placed in the sea waters surrounding Bali. An interesting point of planning in Bali is how to enable eco-friendly interment extensions to villages. This is occurring because of the increasing number of corpses that require cremation thus necessitating no accretions in land provision of graveyards. This research investigates the landscape of death in Bali expressed in its traditional values in the area of planning which implicate sustainable environments and land conservation topics. Other functions of graveyards, as noted by Strangstad ( 1988), include ceremonial and their role as educational tools for history lessons, art, sociology, geology, English lessons, as well as for scavenger hunts.

Mid-Wisconsin to Holocene permafrost and landscape dynamics based on a drained lake basin core from the northern Seward Peninsula, Northwest Alaska

Permafrost-related processes drive regional landscape dynamics in the Arctic terrestrial system. A better understanding of past periods indicative of permafrost degradation and aggradation is important for predicting the future response of Arctic landscapes to climate change. Here, we used a multi-proxy approach to analyze a ~4 m long sediment core from a drained thermokarst lake basin on the northern Seward Peninsula in western Arctic Alaska (USA). Sedimentological, biogeochemistical, geochronological, micropaleontological (ostracoda, testate amoeba) and tephra analyses were used to determine the long-term environmental Early-Wisconsin to Holocene history preserved in our core for Central Beringia. Yedoma accumulation dominated throughout the Early to Late-Wisconsin but was interrupted by wetland formation from 44.5 to 41.5 ka BP. The latter was terminated by deposition of 1 m of volcanic tephra, most likely originating from the South Killeak Maar eruption at about 42 ka BP. Yedoma deposition continued until 22.5 ka BP and was followed by a depositional hiatus in the sediment core between 22.5 and 0.23 ka BP. We interpret this hiatus as due to intense thermokarst activity in the areas surrounding the site, which served as a sediment source during the Late-Wisconsin to Holocene climate transition. The lake forming the modern basin on the upland initiated around 0.23 ka BP, which drained catastrophically in spring 2005. The present study emphasizes that Arctic lake systems and periglacial landscapes are highly dynamic and permafrost formation as well as degradation in Central Beringia was controlled by regional to global climate patterns and as well as by local disturbances.

Understanding landscape and the values of traditional architecture and construction

Ponencia presentada en el congreso internacional organizado por el Comité Internacional de Arquitectura Vernácula de ICOMOS - UNESCO.

Architecture of a Bench-Type Carbonate Lake Margin and Its Relation to Fluvially Dominated Deltas, Las Minas Basin, Upper Miocene, Spain

The Upper Miocene stratigraphic succession of the Las Minas Basin, located at the external zone of the Betic Chain in SE Spain, preserves several examples of lake carbonate bench deposits. Excellent exposures of the carbonate benches allow detailed observation of the architecture of these sediments and provide new insights for the ‘‘steep-gradient bench margin–low energy’’ model proposed by Platt and Wright (1991). The lake carbonate benches developed in close association with fluvially dominated shallow deltas that exhibit typical Gilbert-type profiles. The delta sequences comprise bottomset prodelta marl facies, distal to proximal foreset facies, deposited mainly in a delta-front environment, and topset facies, the latter reflecting both subaqueous delta-front and subaerial delta-plain environments. The development of the carbonate benches was constrained by the convexupward morphology of the deltaic deposits, which led to the available accommodation space for the growth of the steep-gradient platforms. The benches display a progradational pattern characterized by sigmoid-oblique internal geometries and offlap upper boundary relationships, which suggests that the carbonate benches developed under slow though continuous lake-level rise. Both the dimensions of the benches and the dominant carbonate components (i.e., encrusted charophyte stems and calcified cyanobaterial remains), allow comparisons with the progradational marl benches recognized in modern temperate hardwater lakes. Accordingly, the case study presented here provides a good ancient sedimentary analog for low-energy lake carbonate benches. Moreover, the evolutionary trend inferred from the fossil example offers new insights into the depositional conditions of this type of sediment and allows recognition of the transitional pattern from bench to ramp carbonate lake margins.

Transactions of the Department of Agriculture of the State of Illinois with reports from county and district agricultural organizations for the year ...

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Piscataquis County, Maine, 1858 (Image 1 of 2) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Piscataquis County Maine, from surveys under the direction of H. F. Walling; field notes under the direction of L. H. Eaton Esq. civil engineer. It was published by Lee & Marsh in 1858. Scale [ca 1:63,360]. This layer is image 1 of 2 total images, representing the northeast portion of the four sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator projection (UTM Zone 19N, meters, NAD1983). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town boundaries, and more. Relief shown by hachures. It includes many cadastral insets of individual county towns and villages. It also includes illustrations, business directories, and tables of statistics and distances.This layer is part of a selection of digitally scanned and georeferenced historic maps of New England from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates, scales, and map purposes.

Lake George, New York, 1890 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Lake George, Rev. ed., by S. R. Stoddard. It was published by S. R. Stoddard in 1890. Scale [ca. 1:63,360]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Universal Transverse Mercator (UTM) Zone 18N NAD83 projection. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, township and county boundaries, radial distances from multiple points, selected public buildings, private residences with names of property owners, other points of interest, and more. Relief is shown by hachures and spot heights. Includes insets: Ruins of Fort Ticonderoga in 1873 -- [The Narrows Region] -- [Hulett's Landing Region] -- [Floating Battery/Mother Bunch islands] -- [Kattskill Bay] -- [Bolton] -- [Caldwell] -- [Glens Falls Region]. Includes historical notes. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Chicago and vicinity, Illinois, 1953 (Image 1 of 3) (Raster Image)

This layer is a georeferenced raster image of the historic, topographic paper map entitled: Chicago and vicinity, Ill.-Ind. : sheet no. 1 of 3 (Evanston), 1953, mapped, edited, and published by the Geological Survey. It was published in 1957. Scale 1:24,000. The source map was compiled from 1:24,000 scale maps of Evanston, Park Ridge, Arlington Heights, Elmhurst, River Forest, and Chicago Loop, 1953 7.5 minute quadrangles. Hydrography from U.S. Lake Survey Charts 75 (1:120,000), 751 (1:60,000), and 752 (1:15,000). This layer is image 1 of 3 total images of the three sheet source map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Illinois East State Plane Coordinate System NAD27 (in Feet) (Fipszone 1201). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief is shown with standard contour intervals of 5 feet. Depths shown by isolines and soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.