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Copper Minerals

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358                 University of California Publications.
ordinary natrolite. Instead of the usual prisms with square pyramidal terminations there are formed small roof-shaped ridges as shown in plate 34, commonly with curved or more strictly broken roof lines and coxcomb-like groups. These are made up of elements that are bounded by a basal plane and unit prism. The smaller angle of the prism generally projects out into the open cavity. In other words, the tendency is to place the b axis at right angles to the wall. The apex of the roof-shaped form is then a prism edge. The radiate groups are produced by laying the elements together along the diverging basal planes whose intersections are roughly parallel.
More complicated aggregates are common. In certain druses lined with greenish amphibole needles the natrolite occurs as small equant groups looking in the distance as if individual crystals perched on the ends of the amphibole fibres, as shown in figure 2, plate 35. A close examination shows them to be com­plex aggregates in which the tabular elements described above can frequently be observed. This mode of occurrence is undoubtedly closely related to the botryoidal groups which are occasionally found and which are illustrated in plate 36. Under the micro­scope the structure of the natrolite gangue is rather complex. As viewed on a fracture surface or in section, the radiate groups described show divergent strips that are elongated at right angles to the vertical axis. As the axis is perpendicular to the basal plane the elongation in thin section will always be optically negative. This is just the reverse of that usually seen in diverg­ent «natrolite groups and a positive elongation is generally looked upon as a character of diagnostic importance.14
In sections parallel to the base is often seen the twinning described by Lacroix,15 with (110) as twinning plane forming, as it were, a sort of irregular mosaic when viewed with the aid of a gypsum plate.
A group of natrolite crystals, rare for this occurrence, was found showing the normal development of habit and planes. The
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