Somalilandsun: This Paper “A Geological Interpretation of an Air Photograph of British Somaliland” was read at the Nineteenth Annual Meeting of the Society, Hotel Shoreham, Washington, D. C., January 14 to 16, 1953. This paper was a part of the Report of the Photo Interpretation Committee.
FIGURE 1 below shows an air photograph of part of British Somaliland
Three overlapping air photographs, about 1: 35,000 in scale, were used in order that the area could be examined stereoscopically.
The interpretation shows the structure and structural interrelationships of a series of sedimentary beds. In addition, it has been possible to separate the sediments into three main formations and to determine their order of superposition.
The geological interpretation was greatly assisted by the fact that the’ main formations present each have a contrasting lithology and mode of morphological expression.
The oldest formation, number 1, is characterized by a combination of fine and massive bedding, uneven and dissected dip faces, and a tone rather darker than that of the other two formations. Formation 2 can be identified by its large, slabby, and smooth dip faces, which are little dissected, and by its steep scarps. Formation 3 is easily identified by its dendritic drainage and fine bedding with imperfectly developed dip faces.
The geological interpretation was greatly assisted by the fact that the’ main formations present each have a contrasting lithology and mode of morphological expression.
The oldest formation, number 1, is characterized by a combination of fine and massive bedding, uneven and dissected dip faces, and a tone rather darker than that of the other two formations. Formation 2 can be identified by its large, slabby, and smooth dip faces, which are little dissected, and by its steep scarps. Formation 3 is easily identified by its dendritic drainage and fine bedding with imperfectly developed dip faces.
The direction of dip within the formations having been established, it was apparent that the relationships of the three formations to each other was not straightforward. Evidence in the form of erratic dips and scarps and abnormal contacts showed that extensive faulting was present, and the problem resolved itself into determining which contacts were normal and which were faulted.
The interpretation presented explains the relationships between the three formations in a logical manner, and appears to be the only one that can satisfactorily reconcile all the geological observations.
The structure of the area is controlled by normal faulting. Folds can be recognized within formation 3, but they are of minor importance and may be related to small faults where the reversals are abrupt.
Reference was made to a 1: 1,000,000 geological map of British Somaliland and its accompanying report[1] in order to establish the age of the formations recognized on the photograph. Although the scale of the map is too small to allow any direct comparison of the structure, it appears probable that the succession is as follows:
Formation 3-Anhydrite Series.
Eocene
(Banded anhydrite interbedded with limestone layers)
Formation 2-Arnado Limestone.
(Hard, massive and thick-bedded limestone.)
Formation 1-Nubian Sandstone.
Cretaceous
(Sands and quartzites.)
An additional series, the Allahkajid beds (limestones and shales), occurs between the anhydrite and the Arnado limestone. From an examination of the photographs, it appears probable that this series occurs near the base of the scarps that bound Formation 3.
Grateful acknowledgment is made to the Directorate of Colonial Geological Surveys for the loan of the relevant photographs from their collection; to the Air Ministry for supplying copies of these and granting permission to publish them; and to the Directors of Seismograph Service (England) Ltd., for permission to publish this paper.
By By W. E. Johnstone,Seismograph Service (England) Limited,London
