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.

As one swings along, occasional glimpses of the Baraboo River is obtained; rounding a sharp curve a horse-shoe bend is traversed; and two miles farther, at Ableman, the Upper Narrows of the Baraboo River crowd the sky line. As with the gorge at Devil's Lake and the one at the Lower Narrows, this was cut by a stream in ancient geological times, filled with sandstone when the sea intruded, and later was again eroded. Like the remnant of a drift of snow in the late spring, in the gorge is a bed of sandstone deposited by the intruding sea. Along the crest on the opposite side of the river as one rides along, conglomerate may be seen, seeming almost ready to topple to the base below. The cement pebbles tell of waves beating on a far-off shore. On the right of the road, near the upper end of the gorge, stands a picturesque rock resisting the elements, an attractive land mark, carved by the eternal sculptor.

As Reedsburg is neared, fox farms are passed. The wily animals are grown for their valuable pelts.