Description: |
Front: Script at top of postcard reads, Flower beds and fountain on hillside, Winona Lake, Ind.Back: Body of message reads, Dear Mrs. Simms: Am spending a week of my vacation here at Winona, resting, swimming, and taking in part of the good things of the Bible Conference. Have heard some inspiring sermons. Had planned to write you a long letter while here but could not find time. Will try to do so soon. Was about worn out from the [...] weather but [...] I will go home refreshed in body and soul. With love, Myrtle C. Addressed to, Mrs. W.A. Simms, 1502 S. 80th St., Tacoma, Wash. The Hillside or Hillside Amphitheater was constructed on the lake side of the Beyer Home. The facility was built in 1910 utilizing the natural contour of the glacial bowl. Obviously it gets its name from its location. It probably has more negatives than positives. There is no place to go if it rains and the seat surfaces are at the mercy of the weather. Insects have no barriers. The sights and sounds of the surrounding area can be distracting. The platform is small and for years only a small electronic organ was used to assist the singing. There are storage areas under the platform and at one time there were strings of bare light bulbs. However, it was a popular place for afternoon and early evening services. (the Tabernacle was used if it rained) It had a capacity of about 2000 with room for more who brought blankets or folding chairs. Some of America’s greatest preachers and speakers graced the stage. Services were held there daily during the heyday of the Bible Conferences. The venue still exists. |
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Origin: | 1931-08-24 |
Created By: |
C. T. American Art (Published by Winona Souvenir Store, Winona Lake, Ind.) |
Source: |
http://palni.contentdm.oclc.org/cdm/ref/collection/p15705coll8/id/435 |
Collection: |
Grace College - Winona Lake Postcards |
Copyright: |
Contact Morgan Library, Winona Lake, IN for copy and usage permissions |
Geography: |
Winona Lake (Ind.) |
Subjects: |
Flower beds and fountain, hillside |
Further information on this record can be found at its source.