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Read e-book online Advances in space science and technology. Volume 8 PDF

By Frederick I. Ordway

ISBN-10: 1483199665

ISBN-13: 9781483199665

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MC CALL to the principal regional tectonic lineament (Fig. 13). Cruciform and oblique arrangements are also evident in the sector graben patterns of both lunar and terrestrial craters (Figs. 9, 12). These nicks are difficult to separate from what Spurr [17] called "beaks of subsidence" (Fig. 6 ) . Though Fielder [68] notes that some such beaks have a positive topographic reflection, this is easily explained by recourse to the idea of late eruption concentrated within the area of the "beak of subsidence"; it is doubtful that any very complex argument is required to explain these beaks.

This is an enlargement of the central area of Ptolemeus. T h e numerous craterlets situated at the summit of the short septa which form the composite, annular crater wall are evident. Trains of minor craters run out across the floor of the cirque, clearly following lunar grid lineament trends. P h o t o b y H . C . Urey, Endeavour, 1960. systems which he calls the A, B, C, and D systems. In addition, there are systems related to, and localized around, individual maria. These, of which the system radiating from Maria Imbrium is the best known, are referred to as the R l , R2, R3, etc.

Locally, magma has not attained the surface, but the recessive effects are seen at the surface, and in this case we get a faulted rift valley section without significant eruptive association—though deep within the crust there will surely be eruptive manifestations. Sometimes magma has reached the surface in a linear zone, but the secondary faulting is absent. In this case we get what may be called "undeveloped rifts," especially common along narrower zones of activity. The history of various sections of the rift valley system, even in the narrow confines of Kenya, reveals divergence from one locality to another.

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Advances in space science and technology. Volume 8 by Frederick I. Ordway


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