Open-File Report 2006–1058

U.S. GEOLOGICAL SURVEY
Open-File Report 2006–1058

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Table 6. Well-construction characteristics, depth to top of N aquifer, and type of data collected for wells in monitoring program, Black Mesa area, Arizona, 2004–05.

Bureau of Indian Affairs
site No., and (or)
common name 		Date well was
completed 		Land-surface
elevation (feet) 		Well depth
(feet below
land surface) 		Screened/open
interval(s)
(feet below
land surface) 		Depth to top
of N aquifer
(feet below
land surface1) 		Type of data
collected
8T-537 (BM observation well 1) 02–01–72 5,864 851 300–360;
400–420;
500–520;
600–620;
730–780		 290 Water level
8T-538 (BM observation well 2) 01–29–72 5,656 1,338 470–1,338 452 Water level
8T-500 (BM observation well 3) 07–29–59 5,724 868 712–868 155 Water level
2T-514 (BM observation well 4) 02–15–72 6,320 400 250–400 160 Water level
4T-519 (BM observation well 5) 02–25–72 5,869 1,683 1,521–1,683 1,520 Water level
BM observation well 6 01–31–77 6,332 2,507 1,954–2,506 1,950 Water level
1K-214 05–26–50 5,771 356 168–356 250 Water level
1K-225 07–04–54 5,722 251 19–251 210 Water level
2K-300 306–00–50 6,264 300 260–300 0 Water level
2K-301 06–12–50 6,435 500 318–328;
378–500		 230 Water level
2T-502 08–10–59 6,670 523 12–523 25 Water level
3A-28 04–19–35 5,381 358 (4) 60 Water level
3K-311 311–00–34 5,855 745 380–395;
605–745		 615 Water level
3K-325 06–01–55 5,250 450 75-450 230 Water level
3T-333 12–02–55 4,940 229 63–229 24 Water level
3T-508 (Tuba City NTUA 1) 08–25–59 5,119 475 (4) 0 Water level,
withdrawals
3T-546 (Tuba City NTUA 4) 308–00–71 5,206 612 256–556 0 Water level,
withdrawals
4T-523 (Forest Lake NTUA 1) 10–01–80 6,654 2,674 1,870–1,910;
2,070–2,210;
2,250–2,674		 (5) Water level,
water chemistry,
withdrawals
6H-556 12–08–44 5,635 361 310–335 6310 Water level
8A-180 01–20–39 5,200 107 60–107 240 Water level
8A-295 (Kayenta PM2) 300–00–36 5,623 840 268–280;
691–788		 95 Water chemistry,
withdrawals
8K-443 08–15–57 6,024 720 619–720 590 Water level
8T-510 02–11–63 6,262 314 130–314 2125 Water level
8T-522 307–00–63 6,040 933 180–933 480 Water level
8T-541 03–17–76 5,885 890 740–890 700 Water level
9Y-92 01–02–39 5,615 300 154–300 250 Water level
9Y-95 11–05–37 5,633 300 145–300 268 Water level
10R-111 04–11–35 5,757 360 267–360 210 Water level
10R-119 01–09–35 5,775 360 (4) 310 Water level
10T-258 04–12–60 5,903 670 465–670 460 Water level
Chilchinbito PM3 09–25–65 5,950 1,600 1,140–1,570 1,136 Withdrawals
Hotevilla PM1 306–00–57 6,357 1,757 1,500–1,750 1,450 Water chemistry,
withdrawals
Keams Canyon PM2 305–00–70 5,809 1,106 906–1,106 900 Water level,
withdrawals,
water chemistry
Keams Canyon PM3 301–00–76 5,806 1,090 931–1,090 930 Water chemistry
Kits’iili NTUA 2 10–30–93 6,780 2,549 2,217–2,223;
2,240–2,256;
2,314–2,324;
2,344–2,394;
2,472–2,527		 2,205 Water chemistry,
withdrawals
Kykotsmovi PM1 02–20–67 5,657 995 655–675;
890–990		 880 Water level,
withdrawals
Kykotsmovi PM2 10–14–77 5,760 1,155 950–1,155 890 Water chemistry,
withdrawals
Kykotsmovi PM3 08–07–68 5,618 1,220 850–1,220 840 Water level,
withdrawals
Low Mountain PM2 304–00–72 6,123 1,343 1,181–1,262 1,153 Water level
Peabody 2 306–00–67 6,530 3,636 1,816–3,603 728 Water chemistry,
withdrawals
Peabody 6 06–00–65 6,645 3,559 2,047–3,494 894 Water chemistry,
withdrawals
Piñon NTUA 1 02–25–80 6,336 2,350 1,860–2,350 1,850 Water chemistry,
withdrawals
Piñon PM6 302–00–70 6,397 2,248 1,895–2,243 1,870 Water level,
withdrawals
Rocky Ridge PM2 06–26–63 5,985 1,780 1,480–1,780 1,442 Water level
Rough Rock PM5 06–27–64 6,299 1,425 1,175–1,425 1,156 Water chemistry,
withdrawals
Second Mesa PM2 310–00–68 5,777 1,090 740–1,090 720 Water chemistry,
withdrawals
Shonto PM2 05–05–61 6,465 554 485–510;
514-539		 0 Water chemistry
Dennehotso PM2 06–05–64 5,005 675 475-675 8 Water chemistry
Tuba City NTUA 3 310–00–71 5,176 442 142–442 34 Water level,
withdrawals
Tuba City Rare Metals 2 309–00–55 5,108 705 100–705 255 Water level

1Depth to top of N aquifer from Eychaner (1983) and Brown and Eychaner (1988).

2All material between land surface and top of the N aquifer is unconsolidated—soil, alluvium, or dune sand.

300, indicates month or day is unknown.

4Screened and (or) open intervals are unknown.

5Depth to top of N aquifer was not estimated.

6Developed into the D aquifer.

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