Monday August 15-1932 Wea. MON. MAY 31, 1909 Ther. Left for Glenrids and Regmond an enter Glenellis thompsoni. Have Edom for Dactylos- dites and Issus trodes express. At several jus square completely filled with them. Got one good specimen to take along. Hidden are rusty wea- they delimited slate, or muddy dol. that has the Alenrids and Glenellis all in figure 3. Phycho- paria alanci is the most common form. Saw only one brachidord Ruotella edomii and only one Hypolita. Farther E and higher up in the series are more dol. In fact the lower part of the Parker n has more lime dol and impure dol. than elsewhere. In other words, it is a series of micaceous slate with dunes and some of dol. Farther north there is more shale in feet near all is shale. The question now arises in what One Range saw, farther north in three fault series, or is it simply that the Parker n has in broad undulations with distinct zones of dol. In any event what I saw today is not in fault relations. A hot day out in the sun and I perspired bad.