Diagram showing development of shoreline submergence. Strahler, 1960, p. 419.

In arid climates, a distinctive set of landforms develops in flat-lying sedimentary formations: plain, mesa, butte, badlands, cliff, plateau, canyon. Strahler, 1960, p. 455.

Diagram showing the classification of shorelines. (1) Shorelines of submergence: 1A, submerged mountainous coast; 1B, submerged coastal plain, low relief; 1C, fiord coast; 1D,submerged glacial deposits (drumlins). (2) Shorelines of emergence: 2A, coastal plain type, low relief; 2B, steeply sloping type, strong relief. (3) Neutral shorelines: 3A, alluvial fan shoreline; 3B, delta shoreline; 3C, volcano shoreline; 3D, coral reef shoreline. (4) Fault shoreline. Strahler, 1960, p. 418.

A trellis drainage pattern on folds. This resembles the trellis drainage pattern of eroded dipping sediment (slide Box XII-15), but opposing sets of tributaries are shorted and of more equal length than on cuesta topography. Strahler, 1960, p. 473.

Diagram of wedge of the earth showing the major zones and boundaries. Zumberge, 1958, p. 90.

U-shaped and related dunes, varieties, diagrammatic. Odynsky, 1958, fig. 2.

Four kinds of streams associated with eroded dipping sedimentary strata. These form a trellis drainage pattern. Consequent, subsequent, resequent, obsequent streams. Strahler, 1960, p. 451.

Diagram of the formation of various types of kettles. Hutchinson, 1957, fig. 32.

Seep on homocline where oil beds come to the surface. Diagrammatic figure copied from a book.

Diagram showing modes of occurrence of various types of glacial gravels which have economic significance (Thornbury 1956, p. 576).

Diagram of mantle of decomposed rock, topped by soil overlying bedrock. Strahler, 1960, p. 275.

Orogeny. Diagram showing Grigg's dynamic model to simulate the action of subcrustal convection currents and the response of the crust. The stage illustrated shows the development of a crustal downfold (root or tectogene) with outward thrusting near the surface in response to the currents set up by the rotation of the drums. The substartum in the model is very viscous waterglass, and the continental crust is a mixture of heavy oil and sand. Holmes, 1953, p. 412.

Erosional development of horizontal sedimentary strata. The development of cliffs is accentuated here, as is typical of an arid climate. Strahler, 1960, p. 455.

Diagram of 'Bison antiquis' and the Folsom point. Stirton, 1959, p. 521.

Diagram of beaded esker.