Mattson v. Montana Power Co.

2012 MT 318, 291 P.3d 1209, 368 Mont. 1, 2012 Mont. LEXIS 383
CourtMontana Supreme Court
DecidedDecember 27, 2012
DocketDA 11-0413
StatusPublished
Cited by26 cases

This text of 2012 MT 318 (Mattson v. Montana Power Co.) is published on Counsel Stack Legal Research, covering Montana Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Mattson v. Montana Power Co., 2012 MT 318, 291 P.3d 1209, 368 Mont. 1, 2012 Mont. LEXIS 383 (Mo. 2012).

Opinion

JUSTICE NELSON

delivered the Opinion of the Court.

¶1 Plaintiffs are a group of landowners or former landowners with properties on the shores of Flathead Lake and a portion of the upper Flathead River (Landowners). They commenced the instant action in 1999 in the Eleventh Judicial District Court, Flathead County, against Montana Power Company (MPC) and MPC’s successor, PPL Montana, LLC (PPLM).

¶2 The present appeal is the third in the course of this litigation. In Mattson v. Mont. Power Co., 2002 MT 113, 309 Mont. 506, 48 P.3d 34 (Mattson I), this Court upheld the District Court’s denial of PPLM’s motion to substitute the District Court judge. In Mattson v. Mont. Power Co., 2009 MT 286, 352 Mont. 212, 215 P.3d 675 (Mattson II), this Court reversed a portion of the District Court’s order granting summary judgment in favor of the defendants, vacated the District Court’s orders concerning class certification, and remanded for further proceedings.

¶3 On remand, the District Court denied Landowners’ renewed motion for class certification. The sole issue in this appeal is whether the District Court erred in its application of Mattson II to the class- *4 certification question under Rule 23 of the Montana Rules of Civil Procedure. We conclude that the District Court did so err. We therefore reverse and remand with instructions to certify the class, as specified below, and for further proceedings consistent with this Opinion.

BACKGROUND

¶4 Flathead Lake is located in northwest Montana. Covering 191 square miles, it is the largest natural freshwater lake west of the Mississippi. Its two primary tributaries are the upper Flathead River and the Swan River, which enter from the north and east. The lake drains to the south into the lower Flathead River.

¶5 In 1930, the Federal Power Commission issued Rocky Mountain Power Company (RMPC, a subsidiary of MPC) a 50-year license to construct and operate a dam on the lower Flathead River. RMPC transferred the license to MPC in 1938. Construction of the dam (Kerr Dam) began in 1930 but then was delayed due to the Great Depression. It was finally completed in 1938, and commercial operations began in 1939. The dam is located on the lower Flathead River 4.5 miles downstream of the lake’s natural outlet. It regulates the lake’s water level and generates electrical power for customers in Montana.

¶6 In 1976 (four years before the original 50-year license expired), MPC and the Confederated Salish and Kootenai Tribes of the Flathead Reservation filed competing applications for a new license to operate the Kerr Project (the dam, the reservoir, and appurtenant facilities). They eventually reached a settlement under which a new 50-year license would issue to MPC and the Tribes jointly, and MPC would hold and operate the project for the first 30 years (i.e., until 2015), at which point the Tribes would have the option of taking over the project. The Federal Energy Regulatory Commission issued the joint license in July 1985. MPC continued to manage and operate the project until 1999, when it conveyed its interest to PPLM. PPLM has operated the dam since.

¶7 Flathead Lake is fed by snowmelt and by releases from Hungry Horse Dam. 1 Prior to the construction of Kerr Dam, the lake’s water level rose an average of eight feet each year from mid-April to early June due to spring runoff. The average peak elevation was 2,890 feet above mean sea level. The water level then dropped steadily during the *5 summer to a base level where it would remain until the following spring. Under Kerr Dam operations, however, the lake is raised to 2,893 feet (three feet higher than the average pre-dam peak) by June 15 each year, and is maintained at or close to this level through the summer and into the fall. The lake is then lowered gradually over the fall and winter months to 2,883 feet by April 15, at which point spring runoff begins the cycle anew. The dam was operated in substantially the same manner from 1938 to 2007. As described below, PPLM made a relevant change in procedure in 2007.

¶8 Landowners contend that MPC’s and PPLM’s practice of maintaining the lake at full pool (2,893 feet) has caused, and will continue to cause, substantial damage to their properties. They assert that the shoreline of Flathead Lake and the upper Flathead River is continuously being eroded and undercut by such operation of Kerr Dam, resulting in an “ever-widening footprint” of the lake. They explain that erosion is more severe during storms, that storms are stronger in the fall, and that the presence of higher-than-nor mal waves during fall storms produces substantial shoreline erosion and property damage. Thus, Landowners claim that most of the damage to their properties takes place in the fall when the lake is artificially held at or near 2,893 feet. They contend that this practice of keeping the lake at high levels into the fall storm season when shoreline erosion is most significant causes unreasonable and unnecessary damage to their properties.

¶9 There is no question that artificially maintaining the lake at fall pool impacts shoreline properties. In fact, RMPC anticipated this. In a September 1937 letter to the Federal Power Commission, RMPC stated that holding the lake at 2,893 feet for longer time intervals than those which typically prevailed under pre-dam conditions would “affect” lake borderlands and could, for instance, cause “waterlogging of lands beyond the conventional project boundary.” A report issued by the Federal Energy Regulatory Commission in 1984 confirms this prediction. It states that because the lake, from about May through January, is held at high levels which formerly occurred naturally for only short periods (May through July), the delta and nearby islands at the head of the lake have suffered “high level erosion” and have been “progressively reduced in size.” This is due to the fact that the shorelines in these areas “are now subjected to extended periods of wave erosion during times when they were formerly well above the lake level.” MPC conducted its own study of shoreline erosion in the early 1990s, which revealed that the shoreline is retreating at several *6 locations at the north end of the lake “in response to wind-generated waves at the higher water surface elevation.” MPC’s report states that this shoreline retreat is expected to continue as far as 2,100 feet inland on the east side and 1,640 feet inland on the west side before an equilibrium beach profile is reached. “Without intervention, wildlife habitat and developed lands such as the Eagle Bend golf course could be inundated within a few decades.” A 1994 report prepared for MPC by Dr. Mark Lorang (who is now one of Landowners’ consultants in the present litigation) likewise states that “[w]ave energy is the main physical forc[e] responsible for shoreline erosion in Flathead Lake.” Dr. Lorang explains that the higher the lake level and the longer high lake levels are maintained, the more shoreline erosion. “Ultimately, future shoreline erosion on Flathead Lake will depend on how the lake level is regulated.”

¶10 Dr. Lorang has been studying Flathead Lake since 1982, and has been studying shoreline erosion in particular since the mid-1990s.

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Cite This Page — Counsel Stack

Bluebook (online)
2012 MT 318, 291 P.3d 1209, 368 Mont. 1, 2012 Mont. LEXIS 383, Counsel Stack Legal Research, https://law.counselstack.com/opinion/mattson-v-montana-power-co-mont-2012.