En sommer i Finmarken, Russisk Lapland og Nordkarelen: skildringer af land og folk af J. A. Friis

Lisäpainokset: 2. p. 1880 (299 s.).

En sommer i Finmarken, Russisk Lapland og Nordkarelen: skildringer af land og folk af J. A. Friis

Lisäpainokset: 2. p. 1880 (299 s.).

Ethnographisk kart over Finmarken n:o 1 : præstegjældene : I Vardö, II Vadsö, og en deel af III Næsseby og IV Lebesby

Kartta kuuluu A. E. Nordenskiöldin kokoelmaan

Ethnographisk kart over Finmarken n:o 3 : præstegjældene : I Alten, II Koutokæino, III Hammerfest og en deel af IV Skjærvö, V Loppen og VI Maasö

Kartta kuuluu A. E. Nordenskiöldin kokoelmaan

En sommer i Finmarken, russisk Lapland og Nordkarelen. Skildringer af land og folk,

Mode of access: Internet.

Pascaart van de zee-custen van Ruslant, Laplant, Finmarcken, Spitsbergen en Nova-zemla - [Yleisnäkymä - Overview]

1 Amsterdam 1664

Cosmic-ray exposure ages of pallasites

We analyzed cosmogenic nuclides in metal and/or silicate (primarily olivine) separated from the main-group pallasites Admire, Ahumada, Albin, Brahin, Brenham, Esquel, Finmarken, Glorieta Mountain, Huckitta, Imilac, Krasnojarsk, Marjalahti, Molong, Seymchan, South Bend, Springwater, and Thiel Mountains and from Eagle Station. The metal separates contained an olivine fraction which although small, <1 wt% in most cases, nonetheless contributes significantly to the budgets of some nuclides (e.g., up to 35% for Ne-21 and Al-26). A correction for olivine is therefore essential and was made using model calculations and/or empirical relations for the production rates of cosmogenic nuclides in iron meteoroids and/or measured elemental concentrations. Cosmic-ray exposure (CRE) ages for the metal phases of the main-group pallasites range from 7 to 180 Ma, but many of the ages cluster around a central peak near 100 Ma. These CRE ages suggest that the parent body of the main-group pallasites underwent a major break-up that produced most of the meteorites analyzed. The CRE age distribution for the pallasites overlaps only a small fraction of the distribution for the IIIAB iron meteorites. Most pallasites and IIIAB irons originated in different collisions, probably on different parent bodies; a few IIIABs and pallasites may have come out of the same collision but a firm conclusion requires further study. CRE ages calculated from noble gas and radionuclide data of the metal fraction are higher on average than the Ne-21 exposure ages obtained for the olivine samples. As the metal and olivine fractions were taken in most cases from different specimens, the depth-dependency of the production rate ratio Be-10/Ne-21 in metal, not accounted for in our calculations, may explain the difference.

Norway, 1761 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Kongeriget Norge afdelet i sine fiire Stifter : nemlig Aggershuus, Christiansand, Bergenhuus og Tronhiem, samt underliggende Provstier ... forfoerdiget Aar 1761, af O.A. Wangensteen, Capitain ved det Norske Artillerie-Corps ; T.A. Pingeling Junior, sculp. It was published in 1761. Scale [ca. 1:2,700,000]. Covers Norway and a portion of Sweden. Map in Norwegian.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Europe Lambert Conformal Conic coordinate system. 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 drainage, cities and other human settlements, roads, territorial and administrative boundaries, shoreline features, and more. Includes inset: Nordland og Finmarken under Tronhiems Stift.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.