Doherty v. Oregon Water Resources Director

758 P.2d 865, 92 Or. App. 22
CourtCourt of Appeals of Oregon
DecidedJuly 6, 1988
DocketCA A40087
StatusPublished
Cited by3 cases

This text of 758 P.2d 865 (Doherty v. Oregon Water Resources Director) is published on Counsel Stack Legal Research, covering Court of Appeals of Oregon primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Doherty v. Oregon Water Resources Director, 758 P.2d 865, 92 Or. App. 22 (Or. Ct. App. 1988).

Opinion

BUTTLER, P. J.

Petitioners challenge the Water Resources Director’s1 amended order designating 274 square miles near Hermiston as a “critical ground water area,” pursuant to ORS 537.735.2 The Director also divided the critical area into six [25]*25subareas for management purposes and ordered that the withdrawal of water in the subareas be in accordance with the relative priorities of appropriations within the subareas. We review this matter as provided in ORS 183.482. ORS 536.075(2) and (3). Petitioners raise several issues with respect to the establishment of the critical ground water area and also challenge the order on the ground that it unlawfully reestablishes priorities for ground water withdrawal. We vacate the part of the order purporting to reorder water priorities; otherwise we affirm.

The Columbia River Basalt Group is a thick series of accordantly layered basaltic lavas that form a broad plain covering more than 50,000 square miles of Oregon, Washington and Idaho. The Umatilla Structural Basin occupies approximately 2500 square miles of the Columbia River Basalt Group from Arlington east to Athena-Weston and from the Columbia River south to the crest of the Blue Mountains. The proposed critical area lies in the north central portion of the Umatilla Structural Basin. The Director’s order determined, pursuant to ORS 537.735 and ORS 537.730,3 that [26]*26the ground water level in the critical area was declining excessively, that the ground water supply was about to be overdrawn and that the interests of public welfare, health and safety required the establishment of the Butter Creek Critical Ground Water Management Area.

Petitioners assign error to the Director’s decision to treat this proceeding as a continuation of hearings held in 1976 and 1978 concerning the same proposed critical ground water area and his admitting evidence of the entire record of those hearings. We are satisfied that petitioners received notice of the Director’s intention to incorporate the previous hearings’ records into the record of the 1984 hearing, that, although petitioners did not participate in the earlier hearings, they had adequate opportunity to review the records of those hearings in advance of the 1984 hearing and that they were not prejudiced by the inclusion of the earlier hearing records in the record of this proceeding. We conclude that the Director could properly incorporate the records of the previous hearings in this proceeding.4

Petitioners contend that the Director erred as a matter of law in describing the boundaries of the ground water area. ORS 537.735(2) provides:

“The order of the commission shall define the boundaries of the critical ground water area and shall indicate which of the ground water reservoirs located within the area in question are included within the critical ground water area. Any number of ground water reservoirs which either wholly or partially overlie one another may be included within the same critical ground water area.”
<<* * * * *

[27]*27Petitioners contend that that subsection requires that a critical ground water area contain an entire ground water reservoir. Here, the primary reservoir is an underground lake within the Columbia River Basalt Group. We do not agree that ORS 537.735(2) requires that the entire 50,000 square miles of that reservoir be within the designated critical area. There is no requirement that a critical ground water area contain an entire reservoir. It is sufficient that the boundaries of the area can be defined and that the Director indicates which reservoirs are contained within it.

Implicitly, however, the boundaries must define an area that is susceptible to management and control. ORS 537.735(1). Petitioners contend that there is no substantial evidence to support the Director’s determination that the Butter Creek Management Area has such boundaries. We conclude that Ground Water Report No. 30 supports the Director’s finding that the critical area has geological features which permit the approximation of exterior boundaries of naturally occurring impediments to ground water movement, thereby enabling management and control of the area. The same evidence supports the Director’s division of the area into six management subareas, because it shows that the natural impediments to ground water movement tend to minimize the hydraulic effects between the wells located within the different areas.

The Director is authorized to establish corrective controls if he determines that the ground water supply is about to be “overdrawn” or if ground water levels are declining or have declined “excessively,” and if he further finds that the public welfare, health and safety require such controls. ORS 537.735. The Director found “overdrafting” and an “excessive decline” of water levels. The quoted terms are not defined in the statutes, but the Director defined them in his order:

“Overdrawing (overdrafting) of the ground water reservoir occurs when the annual withdrawal of water from the ground water reservoir, together with any natural discharge from the ground water reservoir, is in excess of the natural occurring annual recharge to the ground water reservoir.
“Overdrafting of the ground water reservoir on a year-to-year basis results in a progressive lowering of the static water level (or potentiometric head), measured at the time of the year [28]*28that maximum recovery of the ground water reservoir has occurred.
“Progressive lowering (decline) of the static water level (potentiometric head) in the ground water reservoir beyond the level necessary to provide the capacity to accept available annual natural recharge constitutes excessive decline.”

Petitioners argue that the legislature has delegated to the Director the responsibility and discretion for developing a specific policy for the application of the terms “overdrawn” and “excessive” within the legislature’s general policy stated in ORS 537.5255 and that they are therefore “delegative” terms, the standards for which, it is contended, cannot be developed on a case-by-case basis but must be set out in [29]*29administrative rules. Springfield Education Assn. v. School Dist, 290 Or 217, 228, 621 P2d 547 (1980).

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Related

Crane v. Employment Division
847 P.2d 886 (Court of Appeals of Oregon, 1993)
Doherty v. Oregon Water Resources Director
783 P.2d 519 (Oregon Supreme Court, 1989)
Doherty v. Oregon Water Resources Director
762 P.2d 330 (Court of Appeals of Oregon, 1988)

Cite This Page — Counsel Stack

Bluebook (online)
758 P.2d 865, 92 Or. App. 22, Counsel Stack Legal Research, https://law.counselstack.com/opinion/doherty-v-oregon-water-resources-director-orctapp-1988.