Geothermal waters have been used f o r r e s i d e n t i a l space heating on a l i m i t e d b a s i s i n Thermopolis f o r s e v e r a l decades. These a p p l i c a t i o n s , using s u r f a c e , a r t e s i a n discharge of hot well water v i a s u b f l o o r p i p i n g , may provide u s e f u l , long-term d a t a on p o s s i b l e development problems. D r i l l-h o l e casing corrosion and c o l l a p s e o r mineral d e p o s i t i o n may be r e s p o n s i b l e f o r dec l i n i n g flows i n s e v e r a l wells; excess i v e calcium carbonate d e p o s i t i o n i s known t o be a problem i n c e r t a i n cases.

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Price: Printed Copy A03 Microfiche A01 Codes are used for pricing all publications. The code is determined by the number of pages in the publication. Information pertaining to the pricing codes can be found in the current issues of the following publications, which are generally available in most libraries: Energy Research Abstracts (ERA); Government Reports Announcements and Index (GRA and I); Scientific and Technical

The Peterson quadrangle is located southeast of Ogden, Utah. The major geographic features in and near the map area are Morgan Valley, the northern Wasatch Range to the west, Durst Mountain to the east, the Weber River in Morgan Valley, and lower Weber Canyon cut into the Wasatch Range by the river.

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