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Osmedernyomok a Balaton kornyékén. (Traces of old valleys in the vicinity of Lake Balaton)
Within the research work on geomorphic history the A. considers following problems: what temporal and spatial relations exist between valley traces if there are any| to what present river can old sections related| what significance old valleys have

Research of historical landscape by using old maps with focus to its positional accuracy
Cartography ; Comparative study ; Czech Republic ; Geographical information system ; Historical mapping ; Landscape ; Landscape analysis ; Landscape structure ; Old map ; Středočeský
Old maps are an important historical source for exploring historical landscapes. They are often used as cartographic bases for studying structural changes and reconstruction of land use. This study is concerned with comparison of positional accuracy
of a set of 'old maps' as compared to present-day maps. Determination of positional deviations defines the degree of precision of the old map and its potential for its use in GIS applications. The total of ten unique historical maps in different scales

Old Crow tephra: a new Late Pleistocene stratigraphic marker across north-central Alaska and western Yukon Territory
Alaska ; Amérique du Nord ; Arctique ; Canada ; Etats-Unis ; Géographie des régions polaires ; Old Crow tephra ; Pléistocène supérieur ; Quaternaire zones froides ; Stratigraphie ; Téphrochronologie ; Volcanisme ; Yukon Territory
Old Crow tephra is the first extensive Pleistocene tephra unit to be documented in the northwestern part of North America. It has an age between the limits of 60,000 and 12,000 yr, set by C and fission-track measurements, respectively. Old Crow
tephra has been recognized in the Koyukuk Basin and Fairbanks region of Alaska, and in the Old Crow Lowlands of the northern Yukon Territory, some 600 km to the east-northeast. The source vent is unknown, but these occurrences, considered in relation

Composition structure and disturbance history of old-growth and second-growth forests in Adirondack Park, New York
The A. compares patterns of species composition, size structure, and disturbance in old-growth, hemlock-dominated forests with those characteristics of post-fire, second-growth forests in the Adirondack Mountains in northern New York to document
the persistence of historical events. The composition and structure of old growth were distinctive, but disturbance rates in old growth were similar to patterns in nearby second-growth forest in spite of differences in stand age and past human activity. Together
the old growth and the unmanaged secondary forests enhance landscape diversity.

Utilising space in sheltered housing or fitting a quart into a pint pot : perspectives of architects and older people
The A., using textual analysis of architects' professional discourse and interviews with older people, examines their different perspectives on space utilisation in sheltered housing.

Reference value of old people's hematocrit and geographical factors
The paper provides a scientific basis for a unified standard of the reference value of Chinese healthy old people's hematocrit. It is found that the altitude is the most important factor affecting this reference value.

Old Crow tephra found at the Palisades of the Yukon, Alaska
This paper presents geochemical data that suggest a correlation between this newly discovered tephra and the Old Crow tephra, and provides the first chronologic constraints on the age of Pleistocene sediments at the Palisades of the Yukon.

Stratigraphic context of Old Crow tephra, Holitna lowland, interior southwest Alaska
The purpose of this paper is to document the stratigraphic and paleoenvironmental context of Old Crow tephra at the southwestern limit of its known distribution, thus contributing to interregional efforts to reconstruct Pleistocene paleoclimates

Létezik-e egymillio évesnél idosebb valodi losz? (Is there typical loess older than one million years?)
In recent years ever more characteristic loess profiles have been analyzed in Eurasia by absolute dating techniques. For most of the investigations, the lithologically sensu stricto true loesses are not or hardly older than the Jaramillo event (0.9

Is typical loess older than one million years? in Lithology and stratigraphy of loess and paleosols.
Recent analyses of loesses indicate that the lithologically sensu stricto true loesses are not older than the Jaramillo event (0.9 m.y. B.P.). The features of the so-celled loess-like sediments or loess derivates are summarized. Paleomagnetic

The upper part of Young Loess in Hungary (the Dunaujvaros-Tapiosüly subseries, cca 13-26th. years old) is underlain by the Mende-Basaharc subseries, cca 27-120th. years old. Old loess and interbedded paleosols in Hungary are called the Paks
subseries, the upper part of which is cca 125-210th. years old and the lower part contains the Brunhes/Matuyama boundary. (DLO).

West Old Baltimore Road

Old industries and regional uneven development : the case of the United Kingdom

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