Yamagiwa v. City of Half Moon Bay

523 F. Supp. 2d 1036, 2007 U.S. Dist. LEXIS 96187, 2007 WL 4276385
CourtDistrict Court, N.D. California
DecidedNovember 28, 2007
DocketC 05-4149 VRW
StatusPublished
Cited by4 cases

This text of 523 F. Supp. 2d 1036 (Yamagiwa v. City of Half Moon Bay) is published on Counsel Stack Legal Research, covering District Court, N.D. California primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Yamagiwa v. City of Half Moon Bay, 523 F. Supp. 2d 1036, 2007 U.S. Dist. LEXIS 96187, 2007 WL 4276385 (N.D. Cal. 2007).

Opinion

*1040 FINDINGS OF FACT CONCLUSIONS OF LAW

VAUGHN R. WALKER, Chief Judge.

Joyce Yamagiwa (“Yamagiwa”), brought this action alleging that defendant City of Half Moon Bay (“City”) damaged certain real property that she holds in trust. Doc. # 1-2. The property, known as the Beachwood Property, is located in the City of Half Moon Bay at Assessor’s Parcel No. 048-280-020. Id. Yamagiwa brought a federal claim for inverse condemnation and pendent state claims for inverse condemnation, nuisance, trespass and recovery of amounts paid to finance public improvements. Id.

This case was tried before the court without a jury on June 6, 7 and July 2, 3, 5, 6, 9, 11 and 12. Doc. ## 173-175, 177, 179, 181, 186-188. The court heard testimony from 22 witnesses, including seven expert witnesses, and received into evidence nearly 300 exhibits. The court now makes its findings of fact and conclusions of law:

FINDINGS OF FACT

The Beachwood Property

1. This case involves a 24.7-acre undeveloped parcel of property located in the City of Half Moon Bay, known as Beach-wood (“Beachwood,” or “the Property”). (Ex. 556.) Both sides agree that there are substantial wetlands on the Property. The principle disputed issue is what caused the wetlands to develop and, more specifically, whether a public project constructed by the City was a substantial cause of the development of Beachwood’s wetlands.

2. Beachwood is located on the east (i e, inland) side of Highway 1, north of Highway 92. 1 The Property is roughly rectangular in shape. Its northern border is 1837 feet long, and its western frontage along Highway 1 is 576 feet. (Ex. 75, at 9900122.)

3. To the north of Beachwood lies an undeveloped parcel of property known as Glencree. To the north of Glencree lies a partially developed subdivision known as Grandview Terrace (“Grandview”). (Ex. 425.)

4. To the south of Beachwood lies resi-dentially developed property known as the Newport Terrace/Highland Park subdivision (“Highland Park”). Highland Park contains three streets running east/west: Terrace Avenue is the northernmost street; Silver Avenue is the middle street; and Highland Avenue is the southernmost street. Golden Gate Avenue runs north/ south and connects Terrace, Silver and Highland. It starts at Highland and dead-ends at Beachwood’s southern border. (Ex. 425.)

5. Beginning in 1983, as discussed in detail below, the City of Half Moon Bay constructed a public improvement on and nearby the Property. The project was known as the Terrace Avenue Assessment District (“TAAD”).

Pre-TAAD Topography of Beachwood

6. The pre-TAAD topography on Beachwood is depicted on Exs. 122 and 426 (the latter being a copy of Ex. 122 with the topographic lines shown in alternating colors for emphasis). Ex. 559 is another topographic map depicting Beachwood and surrounding properties in the pre-TAAD condition.

7. Each of these pre-TAAD topographic maps display 1-foot contour intervals on Beachwood as of October 1976. (White, *1041 394:8-13.) A 1-foot contour interval topographic map is a very detailed map, showing all points of equal elevation at one foot intervals. (Weirich, 806:16-24; Huffman, 1510:6-14; Coats, 1325:14-23.) A 1-foot contour interval topographic map is a design-level map that allows an engineer to design the subdivision and calculate quantities of dirt that need to be cut or filled on the property. (White, 324:24-325:12; 392:8-15.)

8. Topographic maps indicate mounds or depressions on the land by closed-loop polygons. Such closed-loop polygons show that the land inside the loop is either higher than the polygon border (hence, a mound) or lower than the polygon border (hence, a depression). When a closed-loop polygon has hachures or tick-marks on the inside of the polygon, this means that the area inside the closed loop is a depression. (White, 394:4-7; Weirich, 861:8-22.) This rule of topographic mapping is sometimes called “The Rule of O’s.” (Huffman, 1509:17-1510:5.)

9. The detailed pre-TAAD topographic map of Beachwood reflects no closed-loop depressions on the Beachwood Property. (Ex. 122; White, 394:4-19; Weirich, 862:3-5.) The pre-TAAD topographic map does, however, indicate a closed-loop depression on the Glencree property to the north of Beachwood. (Ex. 122, White, 393:15-394:7.) The absence of closed-loop depressions on Beachwood shows that the pre-TAAD topography of the Property lacked any such depressions.

10. Instead, the pre-TAAD topography of Beachwood reflected a gently sloping property, with its highest point (elevation approximately 100 feet above sea level) on the eastern border. The eastern slope of the Property — covering roughly the easterly }éth of the land area — descended from the 100' elevation down to approximately 60'. From that point, the elevation descended more gradually to approximately 47'. The lowest point on the Beachwood Property was along its northern boundary with the Glencree property, and the topography on Glencree continued to descend from that point to a low point along Glen-cree’s northern boundary with Grandview, as indicated on Ex. 426. To the west of the low point on Beachwood is a small ridge rising to approximately 50'; and to the west of that ridge, the Property descends to Highway 1 at its eastern border. (Exs. 122, 426, 559; Weirich, 806:13-807:22.)

11. Using the foregoing 1-foot contour topographic maps, Dr. Frank Weirich, plaintiffs expert hydrologist, prepared a digitized, color topographic map of Beach-wood in its pre-TAAD condition (Ex. 836). Dr. Weirich also prepared a digitized topographic map depicting the low point along the northern boundary of Beachwood (Exs. 837, 838).

Pre-TAAD Surface Flows Onto and Off of Beachwood

12. Before the TAAD project was built, there were four areas that contributed surface flows onto and off of Beachwood. The first area was direct rainfall that fell onto the Property. (Weirich, 826:12-16; Coats, 1285:1-13.)

13. The other three areas were off-site drainages, or watersheds, located upslope from Beachwood in the hills to the east, that contributed surface run-off to Beach-wood in heavy storms. (Weirich, 826:17-827:18; Ex. 828.)

14. The first off-site contributing area was a 132-acre drainage basin located south and southeast of Beachwood. This area was designated Drainage Area A by Dr. Weirich. (Ex. 828, Weirich, 828:18-22.) The second off-site contributing area was a 92-acre drainage basin located southeast of Beachwood. This area was designated Drainage Area B by Dr. Wei-rich. (Ex. 828, Weirich, 830:4-10.) The *1042 third off-site contributing area was a small 7-acre drainage basin located northeast of Beachwood. Dr. Weirich designated this area as Drainage Area C. (Ex. 828, Wei-rich, 830:11-21.)

15. While there were many disagreements between the experts in this case, there was substantial agreement regarding the pre-TAAD watersheds and the amount of stormwater delivered to Beachwood from the contributing areas. The pre-TAAD drainages mapped by Dr. Weirich (Ex.

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Bluebook (online)
523 F. Supp. 2d 1036, 2007 U.S. Dist. LEXIS 96187, 2007 WL 4276385, Counsel Stack Legal Research, https://law.counselstack.com/opinion/yamagiwa-v-city-of-half-moon-bay-cand-2007.