• Skuringsmærker og morænegrus eftervist i Finmarken fra en periode meget ældre end "istiden" 

      Reusch, Hans (NGU (1), Journal article, 1891)
      Forkortet: The uppermost Fig. on p.79 shows the low mountains on the north side of the inner part of the Varangerfjord not far from the Russian border. At b and x occurs a little schist. The rest of the moountains consists ...
    • Strandfladen, et nyt træk i Norges geografi 

      Reusch, Hans (NGU (14), Journal article, 1894)
      Forkortet: The western slopes of the Scandinavian peninsula do not generally extend quite to the sea; but we see there low almost level parts, which the author calls the Norwegian coast plain. The figures on pp. 1 and 2 ...
    • Tekst til geologisk kart over fjeldstrøkene mellem Jostedalsbræen og Ringerike 

      Reusch, Hans (NGU (47), Journal article, 1908)
      Forkortet: In the map a distinction has been made between the old Archaean which consists chiefly of granite and gneiss and the Telemark formation (Algonkian) which is colored yellow with red lines. White quartzite and ...
    • Tekst til geologisk oversigtskart over Søndhordland og Ryfylke 

      Reusch, Hans (NGU (64), Journal article, 1913)
      Forkortet: The first section deals with the previous literature on the subject. The geology of the region of the high mountains and the fjords. This region comprises the whole area represented on our map with exception of ...
    • Voss. Fjeldbygningen inden rektangelkartet Voss's omraade 

      Reusch, Hans (NGU (40), Journal article, 1905)
      Forkortet:The Western gneiss region. The lightest red in the map is gneiss, the darkestred is an amphibole-bearing rock, the Evanger diorite, mostly made schistoseby compression; the middle red represents granite the ...