1974 results directly related Exclude narrower terms
Relation of terraces to composite river profile
Part of W.O. Kupsch fonds
Relation of terraces to composite river profile.
Relationship between joint direction and rock types
Part of W.O. Kupsch fonds
Relationship between joint direction and rock types.
Relationship of shear joints and extension of joints to stress
Part of W.O. Kupsch fonds
Relationship of shear joints and extension of joints to stress.
Relationships of sea-floor trenches to earthquakes, volcanic belts and earth gravity
Part of W.O. Kupsch fonds
Relationships of sea-floor trenches to earthquakes, volcanic belts and earth gravity (isostatic anomaly). The example shown in the inset is Japan. Shepard, 1960, p. 174.
Relative movement of tectonic blocks in southern Netherland
Part of W.O. Kupsch fonds
Block diagrams of the relative movement of tectonic blocks in southern Netherlands. Diagram copied from a book.
Relative sizes of living and fossil organisms
Part of W.O. Kupsch fonds
Relative sizes of living and fossil organisms. (Umbgrove, 1943, p. 92).
Relief diagram and map of small fold - Jackfork formation near Amity, Arkansas
Part of W.O. Kupsch fonds
Relief diagram and geologic map of a small fold - Jackfork formation near Amity, Arkansas (Gilluly, Waters, and WOodford, 1952, p. 204)
Relief forms as developed in arid and humid climates
Part of W.O. Kupsch fonds
Relief forms as developed in an arid climate (top) and in a humid climate (bottom) on identical horizontal rock structure.
Remains of mammoth tooth found near Wiseton, Sask
Part of W.O. Kupsch fonds
Remains of mammoth tooth found near Wiseton, Sask. From upper left to lower right: tusk, rught ulna, left femur,left ulna, thoracic vertebra
Repairing earthquake damage on main square, Arequipa
Part of W.O. Kupsch fonds
Repairing earthquake damage on main square, Arequipa. Noted toppled ornament on the top of building.
Residual and transported mantles
Part of W.O. Kupsch fonds
Residual (A) and transported (B) mantles. (A) The mantle was derived from the underlying granite, and is therefore residual, (B) The mantle was deposited on the granite bedrock and is therefore transported. Zumberge, 1958, p.97.
Residual local anomaly, et al.
Part of W.O. Kupsch fonds
Residual local anomaly, interpreted buried valley, cross section, and corresponding theoretical anomaly, central portion of traverse 1, T. 27, R. 23 W. 3. Low point of anomaly corresponds to trend on slide 124. (Hall and Hajnal, 1962)
Restoration of Pleistocene Wooly Mammoth and Mastodon
Part of W.O. Kupsch fonds
Restoration of a Pleistocene mastodon (above) and a Pleistocene Woolly mammoth (below). A tooth of each is shown with a hand for scale. The crowned tooth of the mastodon was suitable for diet of twigs, branches and cones, whereas the infolded structure of the mammoth tooth was more adapted to a grass diet (Zumberge 1958, p. 362).
Retreating margin of Barnes Ice Cap showing ablation moraine and end moraine
Part of W.O. Kupsch fonds
Retreating margin of Barnes Ice Cap showing ablation moraine and end moraine (Goldthwaite, 1951, Jour. of Geol., p. 570.)
Part of W.O. Kupsch fonds
Reykir pumping station for hot water supply. Operation started in 1943. Produces in 112 wells 350 litres per second at 86 degrees C. to supply 60% homes in Reykjavik, thus saving 65,000 tons of coal/year. August 1, 1960.