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which undoubtedly has occurred—would give rise to gypsum.1 The presence of the marl and salt, I hope to show, offers no objection to this explanation; but simply accounts for the aluminous silicates of the alkalies which existed in the original rock masses.3

The facts obtained so far in the examination of these rocks confirm the conclusions suggested by the quartz-crystals ; and both agree with the evidence obtained in the field. It would not be surprising to find on more careful search in this area minerals containing boracic acid.

Summary of conclu- From the study of the specimens the following consions. elusions have suggested themselves to me :—

1. That the gypsum-masses are not of aqueous or sedimentary origin.

2. That they are formed by the addition of water to anhydrite.

3. That the quartz-crystals were formed at a period anterior to the hydration,

but after the formation of the anhydrite.

4. That the anhydrite may have been produced by the action of sulphuric

acid on limestone, the action probably taking place at a high temperature and in the presence of super-heated waters, in the manner in which many igneous rocks have been altered by solfataric action subsequent to their primary consolidation.

Plate I.

Fig. 1. Section of "gypseous" matrix of the bi-pyramidal quartz-crystals. Composed of anhydrite exhibiting pinacoidal cleavage and lamellar twinning (in two crystals); and gypsum in one large crystal ophitically developed around the anhydrite with repeated twinning. From Marf, North-West Punjab. Magnified x 143 diameters. (Seep. 241.)

Fig. 2. Horizontal section of a bi-pyramidal crystal of quartz, showing anhydrite included in small crystals which are, towards the edge, arranged in zonal lines. From Marf. Magnified x 143 diameters. (See p. 232.)

Fig. 3. A rock composed of gypsum and anhydrite, the latter in small crystals drawn out to form a schistose structure. From the Mayo mines, Khewra, (socalled " semi-anhydrite "). Magnified X 143 diameters. (Seep. 241.)

Fig. 4. Section from the same specimen as Fig. 1. The lamellae of gypsum are bent.

Plate II.

Fig. 1. Crystal of anhydrite, the fragments of which have suffered a slight angular displacement (2") by the development of gypsum between the pieces.

1 It is interesting to note that Mr. Mallet has long ago suggested that the gypsum of the Spiti valley has been due to thermo-aqueous agencies (Mem ,Geo. Surv.,Ind., vol v. (1866), p. 157). I have already shown that the earlier stages of hydration of the sulphate of lime are present in the massive anhydrite collected by Mr. Mallet in the Spiti area (ante, p. 240).

* The presence of the Khewra trap in the salt-marl remains as the solitary proof that undoubted igneous action has taken place in this area.

From the matrix containing bi-pyramidal crystals of quartz, Mfirf. Magnified x 310. (Seep. 241.) Fig. 2. Crystal of anhydrite showing cleavage and twinning. T, T and T* are twinned patches in which the cleavage lines and optical characters are at an angle to those in the general mass of the crystal. The directions of these lines are shown in the diagram (Fig. 3). From massive anhydrite, Spiti valley, North-West Himalayas. Magnified x 310. (See p. 241.) Fig. 3. Diagram showing the directions of the cleavage and twinning lines of the specimen shown in Fig. 2.

OA'* _directions of pinacoidal cleavage. QD=most perfect, lying
OD J in the plane of the axis of minimum optical elasticity.

QP J. = traces of gliding planes.

T, T', T"=twin-lamellas in which the cleavage parallel to OB (the most perfect) corresponds to OD of the remainder of the crystal, and OE, the other pinacoidal cleavage, corresponds to OA (least perfect). The angles are shown in the figure. Fig. 4. Crystal of anhydrite showing the two directions of twinning with gliding planes produced by pressure the.centre of which coincided with A. From the massive anhydrite of Spiti, North-West Himalayas. Magnified x 310. (See p. 241.)

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Director's Office) Calcutta, 31st October 1891.

The staff of the Survey is being distributed as follows :—

Lower Burma.Theo. W. Hughes Hughes, A.r.s.m., Superintendent.

P. N. Bose, B.Sc, 2nd Grade Deputy Superintendent. Upper Burma.— C. L. Griesbach, Ci.e., Superintendent.

Fritz Noetling, Ph.D., Palaeontologist.

P. N. Datta,, Assistant Superintendent.

Bengal.—T. D. Latouche, B.a., 2nd Grade Deputy Superintendent.
Punjab.—C. S. Middlemiss, B.a., 2nd Grade Deputy Superintendent.

W. B. Dallas Edwards, A.r.c.s., Assistant Superintendent.

Sub-Assistant Hira Lai.

GEOLOGICAL SURVEY OF INDIA. Holla-nd: Rocks from Salt. Rangfe. Records,Vol=XXIV. PL. 4.

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