Gibraltar Bluff is reached by crossing the Wisconsin River at Prairie du Sac and proceeding along the highway or by leaving the train at the village of Okee and walking a little more than a mile west. Not only does the climb to the top of this imposing eminence give the refreshment and delight bred of an extensive view but the active exercise necessary for the ascent is guaranteed to produce a keen appetite. When the day is fair the climber is rewarded, when he reaches the crest, by a charming outlook which includes a wide expanse of forest, farm and fell, with Lake Wisconsin half-hidden in the distance. The bluff is a well known haunt of the pasque flower or Badger. The geologists have recently changed the names of some of the formations which are exposed one above the other. The names as given in the "Geology of Wisconsin," Vol. II, 1873-1877, and the more recent ones are as follows: Old names-- 1. Soil and drift. 2. Lower Trenton limestone. 3. St. Peter sandstone. 4. Lower Magnesian limestone. 5. Madison sandstone. 6. Mendota limestone. 7. Potsdam sandstone. New names-- 1. Soil and drift. 2. Black River dolomite. 3. St. Peter sandstone. 4. Lower Magnesian dolomite. 5. Jordan sandstone. 6. St. Lawrence dolomite. 7. Mazomanie sandstone. Pine Hollow About a mile east of Kings Corners, almost opposite a rural school and cemetery, the buildings of a farmstead appear to hug a fringe of wood, high bluffs forming the sky line in the immediate background of the picture. Leaving the car at the home of the owner, Walter Welch, a short walk through a grove brings the visitor against the beetling bluffs; solid, silent, eternities of rock. Pine Hollow is hidden away from the dust of hooting cars, and is a delightful spot wild and perfect in its quietude. One may wend his way almost a mile up the sylvan slope along a stream purling in its rocky channel. Reedsburg and Ableman A picturesque drive of some forty miles is the one to Reedsburg, the County Farm, and return. Trunk Line 33 climbs the terminal moraine about a mile west of Baraboo and from this ice-deposited ridge one obtains an extensive view of the upper portion of the Baraboo Valley. When the ice blocked the elongated depression between the two ranges of Baraboo Bluffs, a lake filled the cavity between the hills to the west. Following the retreat of the ice the water cut a gap in the moraine, draining the area covered by the shallow lake.