160000 37° 360000 h Ri o C am 36° Geologic map compilation boundary Rio Gran de Sa n Ju a n R iv er 560000 S A N TA F E COUNTY a 1 23 4 67 89 4100000 5 Santa Fe ve r Ca na dian Ri Albuquerque 35° 3900000 Southern Española Basin 7.5- minute quadrangles Ri iver Pec os R oG ran de 34° 1. White Rock 2. Horcado Ranch 3. Tesuque 4. Agua Fria 5. Santa Fe 6. Turquoise Hill 7. Seton Village 8. Picture Rock 9. Galisteo i ve r 33° 3700000 G i la R Las Cruces 1:5,500,000 0 50 100 Miles 32° 3500000 109° 108° 107° 106° 105° 104° Figure 1–Index map for New Mexico and the study area in the southern Española Basin. 3970000 3960000 3950000 20 0 0' 106° W Figure 3–Select physiographic and tectonic features for the southern Española Basin. 3930000 k r ee ra s- l is t eo C je Ti Ga o yo 3920000 M D E lt El Dorado Lamy CK O DR FER E lt B U I N T to F a u Q i A nc TE X ño a E C rr sA a r co SAN G RE ' F au San CR I STO ' 00 30 30 0 0 ag e 50 0 ' San ta Fe Pla tfor m 0' t Vi l l U PLIF T lt on CE RR ILLO S F au ee k ga Cr au l 0' 35°30' N do oy o o nd o S et rr rF 25 i na al l A ent 25 ym le d 106°10' W ncea e , co Madrid G 0' F a u lt l in Cerrillos 25 Cie ne ba nc 5 Miles ee k a yo H Ar ro Em Sy a nz Turquoise Hill s ll o r ri C e H il ls 5 Kilometers Fe t 0 4 a B on ek Cr e e ta F e R iv Ho n nt ult La B aj ad a Fa pm e n s c ar aE 3 0' jad La Cienega Gal isteo Cr Scale 1:250,000 0 1 2 2 ve r Ri 1 0 0 0 0 0 0 ' ' Fe a t 50 n 0' Sa Sa n Azte c S S y n c p ri n g s l i ne on P de r an ESP AÑ la b OL asa s A Agua Fria 25 Ba n t F au l o 40 0 0' Little Tesuque Creek Santa Fe Ca ' 00 50 r oy Sa La an H ag ent m bay Em BA au te la O M R io G Geologic map compilation boundary Ar WWTP La Cieneguilla Alam o Cr eek Santa Fe Uplands 0' 30 0 0' Tesuque g r o s s in id r o C Sa n Is 35°40' N ha 60 0 ue An c 0' 70 0 uq Tes ada Faults outside compilation boundary (Sawyer and Minor 2006) Las Dos Fau lt Cañ Magnetically defined, lateral limits of Cerros del Rio volcanic field (Grauch and Bankey 2003) Depth contours (ft) to top of Oligocene volcanics, dashed where poorly constrained. (Grauch and Bankey 2003) mbe Rio lt lt ck Na En Medio Tesuque Pueblo F au ny Cerros del Rio volcanic field Ha g a Rio ona F au h Ro Ca Jac 35°50' N Buckman an W i te Nambe Pueblo Pojoaque r m u ck st B o e Rive 420000 SI N JE ME Z UN TAI N S San Ildefonso Pueblo We P a aj t ri 410000 Po joa q u 3940000 400000 MOU NTA I N S 390000 Sample site with database well ID 400 = EB-400 488 Ground water nc h a da A Ca ña Ground water (NMBGMR 2005) Surface water (NMBGMR 2005) Supply well 287 286 289 121 165 096 291 094 600 594 065 610 609 608 098 592 093 588 107 136 466 178 522 208 089 557 Tesuque 554 082 498 497 C 371 297 296 295 495 510 Little Tesuqu e 527 571 526 122 058 110 601 104 596 615 590 611 584 YLM#2 599 367 Creek 494 153 150&474 591 151 473 473 NMOSE 475 011 154 434 141 281 156 piezometer 472 059&598 492 280 277 276 155 493 587 282 279 583 174 Bedrock 123 278 429 476 012 593 604 455 207 149 009 642 A 246 024 148 240 589 505 244 543 550&552 138 537 562 555 477 551 103 008 338 Agua Fria 561 558 559 337 577 409 023 408 535 336 E 542 541 F 415 544&545 414 467 556 595 515&516 533 042 041 413 532 512&513 553 013 014 183 525 549 508 WWTP 363 015 528 172 507 469 529 530 524 r 578 219 020 iv e 458 547 546 410 501 040502 328 eR 548 579 nta F o d 046 406 459 H on 232 Sa oy o 045 Ar r 017 016 329 573 383 359 116 356 569 Cieneguilla 054 460 355 293 131 294 391 582 538 223 354 539 135 386 112 k 323 e 134 e 560 r C 511 a g 339 317-321 457 Cien e 313 370 307 644 315 005 018 G 607 004 383 002 606 La Cienega 019 441 385 605 623 422 521 437 518 001 343 517 640 427 r eek yo 424 za C rr o 435 436 613 on an A B a 509 624 425 462 390 419 l l in El Dorado a YLM#3 G 217 491 214 519 444 412 520 205 449 618 461 439 1 1:215,000 2 3 D E ala ba sas Santa Fe SAN G R E r oy oC re e k 139 452 581 teo C 396 536 420 454 201 4 5 Kilometers 5 Miles 206 622 342 M Sa n s a rc o oyo Ar r 534 Ga l is 468 0 159 285 105 603 612 0 064 639 638 637 636 H Geologic map compilation boundary A 010 086 085 489 Surface water 503 081 635 634 Alamo Creek 633 632 490 585 196 575 160 631 630 629 257 Ar # # # 628 627 626 625 487 576 570 3960000 Sample Locations Ion and Elements 300 299 298 563-568 Tesuque Pueblo Lamy Figure 4– Locations of ground water and surface water samples collected and data compiled for ion and trace chemistry in the southern Española Basin. 3950000 D 597 540 514 3940000 de an 481 482 ue 416 486 483 523 esuq 480 271 3930000 479 484 Tribal Land boundary 478 420000 T Rio 485 270 269 268 Ri 531 506 B 267 266 265 r oG 410000 M OU N TAIN S 400000 C R IS TO 390000 Tesuque Pueblo 196 503 160 ala ba sas 587 596 590 603 YLM#2 R Fe i Santa Fe 493 583 240 589 Agua Fria 338 337 336 v er do Hon oyo A rr Cieneguilla e ga Cr Cien e 386 La Cienega 607 606 605 z Bo n an a Cr ee 415 414 413 501 494 502 ek k 422 YLM#3 Ga 214 Creek 356 582 315 Little Tesuqu e 3940000 nta Sa 495 591 584 599 367 497 297 296 295 WWTP 328 093 588 601 r oy oC Ar 592 498 l l in aA yo rr o 432 436 437 427 424 El Dorado 435 444 449 0 1 2 3 4 5 Kilometers 5 Miles 342 M Sa n s a rc o Ar r oyo 454 teo C 420 Ga l is 0 1:215,000 re e k 439 Lamy Figure 5– Locations of ground water and surface water samples collected and data compiled for stable isotope chemistry in the southern Española Basin. 3930000 nc h a da A Ca ña 594 059 598 Bedrock 600 585 610 609 608 NMOSE piezometer 159 DE Alamo Creek 158x Tesuque 165 S AN G R E 085 3950000 Tribal Land boundary Sample site with database well ID 400 = EB-400 Ground water (NMBGMR 2005) Ground water (NMOSE 2004) Ground water (Anderholm 1994) Surface water (Anderholm 1994) Surface water (Mills 2003) Supply well Geologic map compilation boundary # # # 597 300 299 298 ue Sample Locations Stable Isotopes esuq 267 266 265 T Rio 270 269 268 3960000 Ri o G 621 3970000 420000 M O UN TAI NS 410000 CR IS TO 400000 ran d e 390000 410000 420000 3970000 400000 esu q ue de an Gr F au Ri o an T Ri o c km au lt na F Bu Ja co st We lt 0 2 3 4 ncha da A Ca ñ a 1 5 Miles 5 Kilometers 3960000 Las Dos Fault 1:215,000 0 Tesuque Pueblo Tesuque Alamo Creek General Geology Geologic Units Quaternary alluvium Santa Fe Tertiary Tesuque Formation ba s as oC a la Ar r oy a C r ee 3940000 lt El Dorado 3930000 yo au r ro eF i A na l ag ll Ga Geologic map compilation boundary k V il anticline, certain anticline, approximate anticline, concealed syncline, certain syncline, approximate syncline, concealed La Cienega z Bo n a n Cr eek ton ? Folds ga Ci en e Se i i ? t Proterozoic undivided fault, certain fault, approximate fault, concealed fault, inferred, approximate fault, inferred, concealed fault, queried, approximate fault, queried, concealed do Cieneguilla Paleozoic undivided Faults on yo H aul Arro sF r iso Mesozoic undivided iv e am Tertiary Galisteo Formation R Fe lt nt a Sa ul t F au Tertiary Espinaso Fm R do Tertiary Diamond Tail Fm u lt ing Fa Tertiary intrusive rocks C r os s Agua Fria Tertiary Bishops Lodge S Fe H on idro San Is Tertiary Tesuque Fm mafic volcanic rocks ta an Fa Ch Tertiary Cerros del Rio volcanic rocks r ive 3950000 Quaternary-Tertiary Ancha Formation Ma S an r cos A o r ro y Figure 6–Generalized geologic map of the southern Española Basin (modified from Read et al. 2004). li Ga ste oC k r ee Lamy lithosome B below lithosome A coarser lithosome S oC a la Ttl Ttbl Te Te under Tts Ar Agua Fria lithosome E below lithosome S Ar r Cieneguilla oy o lake sediments ne Ci e Tg Mesozoic/Paleozoic Proterozoic contact uncertain contact approximate contact approximate contact Limits of Ancha Formation Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) See Table 1 for unit descriptions La Cienega lit ho s om lli n Ga lithosome E below lithosome A r ro S an r eek ga C a Bon nz a Cre ek lower-middle lithosome A El Dorado eE aA do yo M 3930000 Tg under Tts Ti and K H on 3940000 Chamita Fm (Tcv) r r sA a r co ro y o Lamy k Tts Tts belowTta iv e r ee Tte below Tta R Fe oC Tte below Tts nt a Sa ste Tte Geologic map compilation boundary Ttb below Tta Santa Fe r oy Ttbfm 3950000 Tccv Ga li Ttafu ba s as Ttacu below Plateau lithosome A below the plateau lithosome A below lithosome S Alamo Creek ncha da A Ca ñ a Tta Ttacu Tesuque finer lithosome S Geologic Units Tta below Tts ue lithosome S below lithosome A su q 2 Kilometers Tesuque Pueblo Te 1 2 Miles lower middle lithosome A o Ri 0 1 coarse upper unit of lithosome A 420000 3960000 Tcv 1:215,000 0 410000 3970000 400000 Tribal Land boundary Gr Ri o an de upper axial river deposits below lithosome A Figure 7– Generalized subcrop map (Quaternary units and Ancha Formation removed) showing the spatial distribution of lithosomes A, B, E, S, and lake sediments in the Tesuque Formation (from Koning and Johnson 2006). 420000 P E Ri o N Tribal Land boundary au 3940000 o El Dorado E K H E T R R N O O C T E Lamy I S Arroyo k a A in ee k Cr ee o Cr Ga lis te za r e ek y aC iver aF d e A E G H o ndo y Arro o ne g n B o na eR r ro E N I C F ta g r e S a n San Fria Sa nt Santa Fe R ive r E V I Agua A N Z A N E K B O R E C io C r i s t o a ab l de ra n G io R S A N TA F E Geologic map compilation boundary a s sa Ga ll te la L ar c o s G A S an M Perennial Ephemeral Cerrillos Bedrock boundary Madrid T H K S O U R E E C T E O L I S A G Galisteo Figure 8–Drainage basins and perennial and ephemeral stream courses in the southern Española Basin. 0 0 1:325,000 2 Miles 2 Kilometers 3920000 P o S A N D O VA L Cochiti L ake er o R ed ad oC oy La Cienega Drainage Basins Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) F E WWTP M be Little Tesuque Creek Cie eo C r eek Ground water divide (from Figure 9) Tesuque ee k r Ar en up Ga li st ver Cieneguilla Tesuque Pueblo Ch e Ri N A io SA T Alamo C r R C A D J E A P R L L A IO T E A U ha ta F S S A nc S an LO O J ja M A D A A H Ñ C A N C añ a d a A Pa A AL R E U UE Q U AQ e S u O io Tesuq O C t ri Ri o am 3960000 T SANDOVAL M o u n t a i n s 400000 eR 380000 400000 410000 420000 3970000 390000 Te su 6900 7000 66 00 00 67 680 0 7100 DI VI DE 3960000 630 0 59 00 580 0 62 00 it 6500 n 640 0 U 57 00 ue D aq 55 00 jo Tesuque Pueblo TE SU QU E En Medio Po 00 56 e uqu Tes 50 61 Rio 54 00 00 61 e- Rio G ran de qu 00 60 B Geologic map compilation boundary Gran C de Unit H la b as a s Ca A Piezometer A r ro yo F E oyo Ar r T N A do Ho n S Cieneguilla El Dorado li s t Un it Lamy r eek Ga eo 6500 M San s A arco o r r oy 6400 6300 6200 6100 600 0 (in feet) yo rro D IV I DE 6150 Depth to Groundwater A 00 69 00 68 700 6 E K CRE ll Ga i na ek it 0 660 O S TE LI GA re a C an z Bon le d G n Cie La Un ega 00 70 n c ea e , co La Cienega Cr eek l in Cie nega Piezometric Head Contours 100-ft 100-ft unconstrained 100-ft closed 50-ft 50-ft closed eo C Cerrillos Ga l ist Gal ist 500 400 300 200 100 20 0 F A Fe E nc Zone of influence Santa Fe well field ta IV Sy Ground water divide Direction of horizontal ground water flow n Sa R DE VI DI R 0 750 0 0 0 74 730 00 72 00 71 Gradient in domestic well pair Downward Upward Neutral E v er Ri A Agua Fria 7600 Downward hydraulic gradient Upward hydraulic gradient eo C r eek Figure 9– Ground water flow conditions in the Tesuque aquifer system, Santa Fe area. 3940000 Supply well 6650 Aquifer Conditions 3950000 Santa Fe 3930000 2 Kilometers Rio ncha 0 da A 1:215,000 1 2 Miles Alamo Creek C añ a 0 7200 Tesuque 390000 400000 342 420 440 324 524 272 810 612 Tesuque Pueblo 30 0 520 242 215 C a ña Tribal Land boundary da 270 a 189 202 222 270 190 255 150 261 181 175 roy o Ca 212 Ar 140 Agua Fria 316 150 130 r 150 125 Rive 385 155 135 Fe ta Sa n 0 30 La Cienega 290 150 166 252 128 180 B on a nz 240 148 156 234 234 182 242 242 188 355 177 162 aC 139 20 TDS isocon 20 Well sample with TDS concentration Surface water sample with TDS concentration Supply well NMOSE Piezometer 300 200 300 TDS concentration 400 in mg/L 500 400 639 320 400 308 50 0 182 231 Ciene 600 448 eek ga Cr 227 (QTa) 368 (Tt) 240 G A i na all y rro o 330 310 468 224 221 243 527 245 186 El Dorado 190 315 274 406 270 546 300 200 170 173 249 1010 2480 300 351 560 335 500 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 400 540 184 176 330 365 374 264 216 do Ho n 233 356 320 132 YLM#3 194 400 00 5 280 380 500 370 2539 (Te) r eek Fe 413 113 226 Little Tesuq ue Creek 390 166 151 147 176 oy o Ar r 274 Total Dissolved Solids (TDS) 132 128 144 162 144 92 154 293 321 110 188 160 350 210 158 200 200 156 186 184 152 350 384 262 200 170 473 260 Santa 373 248 170 296 264 236 252 510 315 290 146 116 150 141 WWTP 164 137 108 191 Cieneguilla 213 200 290 300 310 221 195 152 157 s 160 200 40 0 245 210 180 140 153 156 176 138 123 137 185 260 175 YLM#2 Tesuque 153 202 136 190 344 200 260 306 164 183 161 asa 2 Kilometers 223 185 180 190 192 lab Geologic map compilation boundary 0 220 156 e 260 190 240 210 220 2 Miles 220 239 195 194 216 u qu Tes 410 390 200 Scale 1:200,000 NAD83 1 252 270 A n ch 390 120 Rio 500 3960000 de ra n 186 300 200 400 505 340 320 420 340 Ri oG 132 235 233 516 863 400 135 3950000 500 3940000 0 30 210 220 30 0 570 0 420000 216 311 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic S a an M rcos Ar r oyo 296 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 10–Concentration of total dissolved solids for ground water in the southern Española Basin. 250 40 0 277 453 Lamy 306 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 274 410000 254 30 0 290 108 132 263 400000 418 524 847 610 816 530 1100 90 0 Tesuque Pueblo 0 60 340 325 855 C a ña 544 da Geologic map compilation boundary 280 280 285 325 430 60 0 225 296 265 205 180 800 385 305 255 475 205 230 390 280 250 300 220 260 30 0 240 350 807 Santa 260 357 260 230 YLM#2 280 450 160 270 250 371 336 445 230 235 235 304 333 175 475 556 215 265 766 230 313 353 347 423 311 688 Agua Fria 341 683 150 236 556 270 194 320 253 550 255 209 210 273 295 660 205 110 171 292 230 348 224 WWTP 559 540 0 181 0 221 6 320 290 Fe lab asa s 275 440 Ar 60 0 roy o Ca 309 n Sa 235 R Fe ta r ive 30 0 254 230 220 225 240 546 La Cienega 440 230 239 235 400 399 401 324 400 398 354 60 0 Conductivity (Cond) 449 --- 30 0 290 30 0 Supply wells NMOSE Piezometers G 376 r eek in all 380 aA yo rro 776 550 371 417 339 271 601 El Dorado 876 392 526 706 380 901 900 248 420 407 1550 549 2720 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 405 406 286 90 0 461 471 432 Specific conductance 20 1104 360 540 200 isocon Well sample with specific conductance Surface water sample with specific conductance 516 928 eek za C r YLM#3 235 742 460 do 258 ga C Ciene 216 Bonan 229 322 648 415 213 210 545 Ho n oy o Ar r 229 410 300 Specific 600 conductance 900 in µS/cm 353 304 390 220 Cieneguilla Little Tesuq ue Creek 228 284 30 0420 301 e 30 0 250 260 Tesuque 435 u qu Tes a 420 289 279 262 294 2 Kilometers 290 303 305 305 410 325 285 280 280 Rio 380 300 280 290 290 260 300 A n ch 0 Tribal Land boundary 360 300 380 Scale 1:200,000 NAD83 2 Miles 347 325 3950000 oG Ri 285 30 0 841 30 0 de ra n 300 460 460 580 530 1 365 510 1410 250 0 371 351 3960000 985 1280 420000 3940000 673 410000 325 443 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic San M s arco Ar r oy o Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 11– Specific conductance for ground water in the southern Española Basin. 0 60765 Lamy 513 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 457 3930000 455 180 175 405 60 0 390000 A. B. C. D. Fi gur e1 2 Pl o t so f t o t a l d i s s o l v e ds o l i d sv e r s u ss p e c i f i cc o n d u c t a n c e f o r : ( A)a l l wa t e rs a mp l e s ; ( B) T e s u q u eFo r ma t i o n g r o u n dwa t e r ; ( C)Es p i n a s oFo r ma t i o ng r o u n dwa t e r ; a n d ( D)Emb u d oFo r ma t i o ng r o u n dwa t e r . 390000 400000 23 15.0 19.9 410000 21.6 18.8 19.3 22 Tesuque Pueblo 18 26.1 24 24.3 29 Ri oG 27 19 e Geologic map compilation boundary 18.6 23.2 20.9 19.5 YLM#2 16.2 s asa lab 16.4 16.3 roy o Ar 16.9 17.2 14.9 14.2 Fe 16.2 La Cienega 18.3 14.4 do Cr eek 20.3 20.5 --- 19 YLM#3 18.2 G i na all A rro 14.3 19 yo 17.9 19 20.3 18.7 25 18.9 18 NMOSE Piezometer 17 17.3 16 19.8 19 Isotherm 20 El Dorado 19.5 Temperature in °C Well sample with temperature Surface water sample with specific temperature Supply well 17.2 21.1 18.5 Temperature 15 19 22 Cr eek iene ga 18.7 Bonanza 15 22.5 16.5 23.1 19 22 C 11.2 15.3 14 12.8 20 17.4 11.9 18.9 16.1 15 16.7 14.4 17.5 15.5 16.8 Ho n oy o Ar r 18 20.6 13.7 13 Fe 16 15 16.4 Cieneguilla 16.1 15 22.2 19.6 nt a 15.1 16 16 13.7 Agua Fria 16.3 18.0 15 14 23.2 Santa 13.2 12.8 10.5 13 17.4 17.9 17.2 20.4 Sa Little Tesuq ue Creek 19.8 23.2 WWTP 14 r 17 Rive18.5 18 18 14.2 12.9 18.2 18.9 27.5 15 17.3 21.8 18.8 20.4 19.8 19 16.3 18.9 16 Ca 2 Kilometers 18 15.9 19 Tesuque 18 u qu Tes 0 17.9 25.1 20.8 22.1 25.5 2 Miles 14.4 Rio 20.9 22.9 22.7 23.5 Tribal Land boundary 19 17 27.2 Scale 1:200,000 NAD83 13.9 16.5 21.7 23.4 24.7 28.9 1 15.3 17 3960000 ra n 21.5 18.1 20.8 20.7 3950000 ha 3940000 nc 15.8 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 16.1 San Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic Figure 13–Temperature of ground water in the southern Española Basin. rco Ma sA r r oy o Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) 15.9 Lamy Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 A 15 da 15 ña de Ca 19 18.6 0 420000 400000 7.8 410000 7.7 7.3 8.1 7.5 7.6 7.2 7.6 7.2 8.1 7.4 7.9 7.3 Geologic map compilation boundary 8.2 8 8.2 8.1 8 asa roy o Ca lab 7.6 7.7 8 Ar WWTP n Sa 8.2 7.6 7.8 ta R Fe 8.1 Cieneguilla 7 8 7.3 8.2 7 8.2 7.9 6.5 8.2 8.1 6.9 7.8 7.4 8.2 8.2 7.8 7.8 87.8 7.5 Santa 7.7 8 7.7 77.57.8 7.8 8.4 8.7 8.1 8.2 7.7 8.7 8 8.5 9.3 7.8 8.5 8.3 8 7.1 8.1 8.1 7.9 8 8.8 8.1 8.2 7.8 7.9 B o na n eek za C r YLM#3 Ga lli n 20 Well sample with pH Surface water sample with pH Supply wells NMOSE Piezometers aA yo 7.7 7.7 7.7 7.9 8.2 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 8.2 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic Figure 14– pH for ground water in the southern Española Basin. S a an M rcos Ar r oy o 7.9 7.7 El Dorado 8.9 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) 8.3 7.6 8 8 7.5 7.4 7.3 7.5 8.6 8 7.3 7.3 7.8 7.5 7.2 7.8 8.4 8.3 7.4 3960000 7.5 7.7 8 7.5 7.4 7.5 9.2 rro 7.7 7.9 7.3 7.8 7.3 7.5 7.8 pH isocon 7.7 8 8.1 8 7.4 7.4 7.7 pH 7 7.5 pH in standard units 8 8.4 6.9 7.6 8 eek ga Cr Ciene 9 8.4 8 8.7 7.8 8 7.6 Fe 7.7 7.4 7.9 oy o Ar r 7.8 7.9 8 7.9 7.9 8.4 8.3 8.2 7.8 8 9 7.1 7.2 7 7.6 7.9 7.9 8 8.1 7.3 8 7.3 7.9 7.9 8.2 8 8 7.9 8.1 8.2 8 8.1 do 7 Ho n 7.3 8.2 6.9 7.5 r 6.7 ive 6.7 8 8.2 8.5 8.9 7.6 Little Tesuq ue Creek 8 7 7.4 8.3 6.9 7.5 8.1 Agua Fria 8.4 8 7.8 8.8 8.2 7.9 7.9 8.1 8 8 8.2 8 6.9 8 8 7.3 YLM#2 8.1 s 9 8 7.6 8 7.7 8.3 7.7 7.7 7.5 7.1 8 8.3 7.3 8.1 8 8 8.1 e 6.4 7.7 8 8 8 8.8 7.7 7.4 La Cienega 7.9 Tesuque 8.1 7.8 3950000 8.1 8.1 n cha 2 Kilometers 7.7 8.3 7.9 u qu Tes 8.3 8.6 8.5 8.6 8.5 8.3 8.5 8.4 7.7 da A 0 2 Miles Tribal Land boundary 7.9 C a ña 1 7.6 Rio 8.4 8.6 8.8 7.6 3940000 ra n oG Ri 8.4 8 8.2 0 7.8 7.9 7.9 7.9 8 8 8.6 8.5 8.8 8.6 7.6 8 Tesuque Pueblo 8 8.1 8.1 7.8 Scale 1:200,000 NAD83 420000 7.8 8.4 8 7.9 Lamy 7.8 8.1 7.6 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 7.6 de 8 9.2 8.8 8.3 7.5 9.2 7.5 390000 100 Percentage of total ions, in milliequivalents per Liter (meq/L) 80 80 Su lfat e m lciu Ca um esi 40 40 agn Ch lor ide + +M 60 60 20 20 0 0 100 0 100 0 ica r +B Mixed-anion 40 Ca m siu tas rbo nat e e Po Ma lfat m+ Mixed-cation 60 Su diu gne siu m So 40 60 80 bon ate 80 20 20 0 100 100 80 60 Calcium 40 20 0 0 20 40 60 80 Chloride Figure 15–Piper diagram showing water types for all ground water and surface water samples from the Santa Fe area. 0 100 Tribal Land boundary ue aA ad Tesuque Pueblo nch a Na-Ca-HCO³ Na-Ca/mixed anion Na-HCO³ Na/mixed anion Tesuque Alamo Creek Mixed cation/HCO³ Mixed cation/SO Geologic map compilation boundary ba s as oC a la r oy Bedrock Santa Fe Ar Supply well Piezometer S ANG R E Mixed cation/ mixed anion iv e Agua Fria r Ar r oy o H on do 3940000 R Fe nt a Sa Creek D E Little Tesuq ue CR I ST O M O U NTAI N S ra n Ri o G esu q ñ Ca Ca-HCO³ Ca/mixed anion Ca-Mg/HCO³ Ca-Mg/mixed anion Ca-Na-HCO³ Ca-Na/mixed anion T Ri o Water Types 3970000 420000 3960000 410000 3950000 400000 de 390000 Cieneguilla eek ga Cr Ci en e a C r ee in aA r ro yo El Dorado 0 1 2 3 ste o 4 5 Kilometers Ga li 0 1:215,000 Cr eek ll Ga k 5 Miles S an M r sA a r co ro y o Lamy Figure 16– Water types of ground water and surface water samples in the Tesuque Formation and bedrock units in the southern Española Basin (based on the piper diagram of Figure 15). 3930000 z Bo n a n La Cienega 100 80 80 Su lfat e m lciu Ca um esi 40 40 agn Ch lor ide + +M 60 60 20 20 0 0 100 0 100 0 ica r +B Mixed-anion 40 Ca m siu tas rbo nat e e Po Ma lfat m+ Mixed-cation 60 Su diu gne siu m So 40 60 80 bon ate 80 20 20 0 100 80 60 Calcium 40 20 100 0 0 20 40 60 80 0 100 Chloride Figure 17– Piper diagram for ground water samples from Proterozoic granitic rocks of the Embudo formation. The dominant water type in the Embudo formation is calcium-magnesium-bicarbonate, with minor enrichment of sulfate and chloride. 100 80 80 Su lfat e m lciu Ca um esi 40 40 agn Ch lor ide + +M 60 60 20 40 20 0 EB -6 0 0 0 100 bon ate ica r +B rbo nat e EB Ca -201 m siu tas Ma e Po Mixed-cation 40 60 lfat m+ 60 80 Su diu gne siu m So EB -3 80 39 EB -4 60 100 Mixed-anion 40 20 20 0 100 60 80 40 100 0 0 20 20 60 40 Calcium 0 100 80 Chloride Figure 18–Piper diagram for ground water samples from the Ancha Formation. The dominant water type in the Ancha Formation aquifer is calcium-sodium-bicarbonate. Sodium enrichment is probably associated with mixing of ground water from adjacent formations, as in samples EB-201, EB-339, EB-460 and EB-640. 100 80 80 te ulfa +S m+ lciu Ca 60 60 ide lor Ch um esi gn Ma 40 40 20 -46 9 20 0 EB 0 J 0 100 -21 7 0 EB 100 ona arb Bic Mixed-anion 40 m Ca rbo nat e+ 449 EB- siu Ma gne siu 0 100 e tas Po 20 lfat m+ Mixed-cation 60 Su diu m So 60 40 80 te 80 20 J 80 60 Calcium 40 20 100 0 0 J 20 40 60 80 Chloride Figure 19– Piper diagram for ground water samples from the Espinaso Formation ( ), Espinaso/Embudo Formation (J) and other Tertiary volcanic rocks ( ). The dominant water types in these volcanic and volcaniclastic formations are calcium-sodium and sodium-calcium bicarbonate, with occasional enrichment of sulfate. 0 100 17 48 84 91 Ca ña da An cha ra n 68 25 27 21 Ri oG 39 14 17 34 Geologic map compilation boundary 30 30 31 asa roy o 35 Ar 28 Agua Fria 27 30 29 Cieneguilla Sa nt a R Fe r ive 38 30 12 29 40 30 39 28 32 53 45 24 24 22 33 54 25 34 79 26 31 61 31 16 37 50 41 48 23 15 8 77 5 0 33 38 97 50 10 0 29 53 134 21 16 2 19 32 36 33 ga Ciene B o na n eek za C r YLM#3 G A 2 y rro 71 47 Cr eek i na all o 50 65 50 43 45 21 44 42 81 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 65 64 120 56 10 0 100 119 100 57 117 56 30 7 41 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic 59 48 34 32 48 71 El Dorado 32 46 40 81 83 59 10 0 194 31 350 50 Ca isocon 62 82 63 45 35 50 Ca concentration 100 in mg/L NMOSE Piezometer 102 68 11 33 38 53 54 32 53 54 30 74 72 31 39 Calcium (Ca) Fe 98 28 24 19 do Ho n oy o Ar r 47 Well sample with Ca concentration Surface water sample with Ca concentration Supply well 83 53 61 56 33 29 20 50 34 65 48 58 57 100 Little Tesuque Creek 50 51 32 36 2 18 43 33 95 41 48 51 134 Santa 51 50 50 66 21 43 7 51 47 69 76 9 2 42 29 27 39 44 44 41 11 24 42 54 40 44 49 50 WWTP La Cienega 43 32 30 31 39 41 28 23 YLM#2 s 24 36 47 31 30 27 33 27 39 27 31 22 11 2 16 38 33 36 Ca 18 37 22 16 17 7 27 31 7 7 33 Tesuque 73 42 39 lab 2 Kilometers 37 4 34 49 45 65 40 e 0 30 33 17 Tribal Land boundary 11 u qu Tes 37 17 17 10 16 50 61 Rio 30 22 20 24 39 38 22 11 2 Miles 13 25 16 47 Scale 1:200,000 NAD83 1 30 25 27 18 35 50 0 49 52 Tesuque Pueblo de 36 35 50 420000 3960000 39 410000 3950000 14 400000 3940000 7 35 0 3 4 20 20 M San arco sA r r oy o 2 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 20–Calcium concentration for ground water in the southern Española Basin. 42 38 43 26 40 Lamy 23 67 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 390000 390000 400000 145 92 Ca 56 ña d aA n ch Tesuque Pueblo a ra n oG Ri 40 51 18 15 37 39 38 Scale 1:200,000 NAD83 13 71 92 39 22 13 30 50 24 31 20 asa 20 9 n Sa 51 67 La Cienega R Fe 69 7 ve r 41 19 22 27 23 6 10 4 21 11 44 39 16 8 24 10 12 Ciene 93 824 Sodium (Na) YLM#3 20 190 Little Tesuq ue Creek 20 88 24 10 7 4 34 6 6 19 36 7 3 7 150 90 25 28 50 16 22 22 22 22 18 9 do 33 25 30 10 85 rro 24 14 Cr eek 59 13 8 19 45 eek ga Cr lli n Ga 29 17 6 aA Santa Fe yo 23 20 15 20 22 40 20 15 21 40 El Dorado 12 20 46 52 33 29 43 14 10 concentration 20 Na in mg/L 40 25 35 25 15 18 34 68 110 210 44 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 26 61 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic S a an M rcos Ar r oyo 100 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 21– Sodium concentration for ground water in the southern Española Basin. 26 13 38 15 28 22 20 Na isocon NMOSE Piezometer 13 20 9 Ho n 50 32 Bonanza 17 40 62 25 21 26 9 24 25 30 22 24 20 25 Surface water sample with Na concentration Supply well 5 10 6 7 13 9 34 39 21 9 oy o Ar r 27 Well sample with Na concentration 6 5 5 8 6 34 20 5 5 5 44 5 19 5 3 4 18 8 58 32 13 59 13 17 11 9 i 19 Cieneguilla 77 ta YLM#2 12 21 7 10 5 WWTP 10 14 11 9 10 33 8 11 Agua Fria 7 54 125 8 39 9 4 7 13 Ar 50 Tesuque 14 23 14 15 s 32 15 lab 2 Kilometers 30 7 8 7 7 16 Ca 0 2 Miles 85 17 61 10 8 17 30 roy o 1 74 28 5 28 24 39 Geologic map compilation boundary 0 23 26 51 27 20 12 e 72 68 70 47 14 14 u qu Tes 57 Tribal Land boundary 63 Rio 120 120 68 7 20 105 51 100 40 83 160 99 73 20 50 45 170 275 11 19 3960000 96 de 53 76 100 420000 3950000 178 410000 3940000 82 90 170 66 127 Lamy 24 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 32 3930000 58 42 37 88 180 310 400000 0.1 nc Tesuque Pueblo ha 0.1 0.1 ra n oG 0.6 Ri 1 1 3.1 0.3 0.2 0.2 Geologic map compilation boundary 0.5 1.4 1.7 3.2 2.3 0.5 asa 3.7 3.6 3.4 R 0.6 2.4 Fe ta Sa n 0.9 La Cienega 0.5 1 0.2 1.3 2.9 1.3 1.4 0.9 0.9 1.2 4 0.9 2.7 1.7 5.8 24.6 1 5 1.3 5.2 4.2 0.2 0.4 2.1 2.5 2.6 2.4 1.2 2.8 2.6 0.7 2.2 2.2 3.2 3.6 6.7 Ca:Na Ratio 20 NMOSE Piezometer G 0.8 1.9 2.1 rro 0 yo Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic oy o 2.1 4.3 4.3 3.1 12.3 5.2 3.4 3.2 2.9 3.3 2.3 2.6 El Dorado 3.3 2 2.9 6.4 4.3 1.7 0.2 0.6 0.7 0.5 0.2 Lamy 3.2 Fault, certain Fault, approximate Fault, concealed Syncline, concealed Figure 22– Ratio of calcium to sodium concentration (meq/L) for ground water in the southern Española Basin. 5.3 3.5 4.2 0.2 0.9 3.5 5 4.6 0 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) 5 2.8 3 3.9 3.3 2.8 0.6 0.5 1.4 2.9 5 1.4 S 2.9 2.2 1 0.9 9.6 2.6 5.9 1 Ar r 2 0.8 1 0.9 12.8 1.6 rcos 6.6 4.7 4.6 do 0.7 a an M 5 3 3.8 eek YLM#3 Ca:Na ratio isocon Well sample with Ca:Na ratio Surface water sample with Ca:Na ratio Supply well 1.3 1.3 0.8 eek ga Cr Ciene A i na all Santa Fe 6.7 2.5 0.5 1 Ca:Na ratio 2 5 Little Tesuq ue Creek 0.3 0.6 Bonanza Cr 0 1 0 2 1.4 5 0.06 0.03 6.4 Ho n oy o Ar r 1 1 4.8 5.7 7 2 0.7 5 3.9 r 0.4 ive 1.4 Cieneguilla 0.6 3.7 0.2 0 WWTP 3.9 9.3 7.3 2.5 12.3 9.2 17.6 6.2 9.2 19.6 Agua Fria 5.4 1.4 3.7 10.6 4.6 5.1 5.1 14.4 1.4 2.1 5.3 6.4 4.7 6.7 roy o Ar 2 0 3.2 12.7 13.9 8.9 7.2 16 7.5 8.6 2.4 16.2 1.7 8.6 10.8 16.1 1 10.5 4.2 7.9 2 16.3 12.1 4.5 lab Ca 0.4 3.8 1.9 1 2.3 0.8 3.7 2.9 3.9 4.1 2 0.9 2.2 YLM#2 s 1.3 2 0.3 e 1 5.6 3.2 1 0.7 7.4 u qu Tes 1.2 5.7 7.5 4.7 3.1 1.5 0.1 0.1 0.6 2.7 1 Tesuque 1.7 5.5 2.6 0.1 3.7 6.2 4 Rio 0.6 0.2 3.3 5 2 Kilometers 11.2 1.7 0.1 1.4 3.7 5 2 Miles 1.7 0.2 5 0 1.6 1.8 0.7 1.4 5 1 0.5 0.3 0.3 0.2 0.4 0.3 0.2 3.9 Tribal Land boundary 1.1 Scale 1:200,000 NAD83 0.3 3.6 2 0.3 0.5 0.3 0.9 0.2 0.4 0.2 0 0.5 0.6 0.7 5 1 3960000 A 3950000 da de ña 5.5 3 2 Ca 420000 0.5 0.5 0.2 0.1 0.6 1 1 0.8 1.1 0.2 0 0.1 0 0.1 0.1 410000 3940000 0.7 1.5 3930000 390000 400000 An Geologic map compilation boundary 3.3 0.6 0.7 1.9 3 4.4 4.2 asa Ar 2.7 0 0 5 WWTP 4.6 3.6 3.2 5 6.9 7.8 n Sa ta R Fe 16 r ive 2.7 2.3 3.1 2.9 4.9 6 2.4 5.2 10.6 6 6.8 3.4 0.9 0.9 7 Agua Fria 5.8 10.6 3.6 5 7.3 1.9 4.2 5.6 3.9 0 5.8 5.9 2.9 0.9 4.3 6.3 5.3 4.2 4.4 4 0.4 2.8 0.5 6.5 6.5 6.4 6.5 6.5 6.4 1.7 2.7 1.2 0.5 2.1 5 10 20 30 20 Well sample with Mg concentration Surface water sample with Mg concentration Supply well NMOSE Piezometer B o na n 28 4.2 13 13.5 9.9 13.5 do 5.8 rro yo 10.8 8.9 6.4 7.7 2.6 8.9 52 110 7.4 6.1 30 14.7 20.1 28 16 18 o 0.6 9.4 16.1 16.1 6.8 18 El Dorado 12 9.7 12.7 15 19 11 7.3 15 6.7 6.4 Lamy 2 10.6 12.5 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 23– Magnesium concentration for ground water in the southern Española Basin. 27 11 9.2 1.1 7.1 4.3 rcos 17.9 12.3 39 10 17.7 8.8 Ma 10 15 7.8 5 San 18.5 20 0 oy Ar r 9.3 9.1 eek za C r lli n Ga Fe 15.4 eek ga Cr aA 20 7.4 15.3 6.5 9.3 5 7.6 5.5 8.5 Santa 5.3 6.1 5.2 4.9 5.3 6.3 4.2 2.8 5.1 3.2 4.2 16.2 0.2 0.1 5.8 7.8 20 Mg isocon 20 Ciene Little Tesuq ue Creek 5 6 30 Mg concentration in mg/L 3.6 4.2 4 YLM#3 7.6 0.7 2.6 5.4 0 3.6 5 14.6 3.8 5.2 2.8 2.1 1.5 Ho n oy o Ar r 12.1 Magnesium (Mg) 4.2 3.4 6.7 8.7 2.7 3.6 3.2 3.3 0.1 1.5 17.3 La Cienega 0.1 3.3 Cieneguilla 10 4.5 lab roy o 5 3.9 8.2 5.8 4.7 Ca 2 3.2 3.8 2.9 6.4 1.6 YLM#2 s 3 5.2 2.9 3.4 4.1 3.4 5.8 3.6 4.2 5.3 4.5 4 5 4.2 Tesuque e 2 Kilometers 0.5 7.4 3.4 5.1 7.7 3.9 5.5 4.8 6.5 5.6 5.7 u qu Tes 3.5 0 5.1 0.5 5.2 Rio 0 8.8 2.7 4.8 2.9 0.9 0 2 Miles 0.8 0.8 4 2 1.2 0.6 Tribal Land boundary 5 5 cha 2.3 3.6 4.1 1.1 5 7.9 4.7 3.2 3960000 Ri 0 7.1 3950000 10 de oG ada ra n Cañ 4.7 5.7 6.4 Scale 1:200,000 NAD83 1 2.8 2.4 2.1 11 2.4 0 3.7 3.1 3 5.7 9.4 9.5 Tesuque Pueblo 30 20 2.8 5.5 6.6 2.6 7.2 7.1 13 3.9 36 3940000 7.2 420000 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 2.1 410000 10 0.4 2.4 0 0 0 20 390000 400000 da A nc ha 495 865 155 ra n 269 330 306 144 150 175 220 159 300 318 175 150 165 121 138 293 120 130 122 145 145 134 YLM#2 276 103 96 54 136 117 130 394 160 Santa Fe 147 154 150 100 135 210 122 150 158 49 185 122 153 135 120 120 135 112 100 116 128 179 205 110 125 147 160 67 67 207 134 100 124 181 Agua Fria 102 95 207 139 150 237 106 121 96 126 160 275 108 242 125 35 93 171 87 118 140 125 106 124 323 151 267 102 WWTP 225 106 135 108 281 174 151 r e 102 113 iv 159 196 93 eR 115 t a F do 138 372 155 n Ho n o Sa 154 y o rr 146 180 Little Tesuq ue Creek 145 160 lab 120 Cieneguilla 283 300 119 125 149 314 La Cienega 150 113 68 120 242 132 87 142 142 128 144 152 122 150 144 150 140 185 183 167 185 184 130 149 126 185 123 134 203 231 138 149 121 eek za C r 197 231 YLM#3 155 a lli n Ga A 170 rro 265 340 146 yo 184 188 194 191 277 213 220 323 198 220 117 244 293 300 HCO3 isocon 303 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 288 133 156 150 Alkalinity 300 mg/L HC03 Well sample with HC03 concentration Surface water sample with HC03 concentration Supply well NMOSE Piezometer 193 155 El Dorado 130 Bicarbonate (HC03) 264 246 339 136 148 183 143 20 256 156 eek ga Cr Ciene B o na n 342 15 0 A 121 187 309 0 30 110 254 3940000 Ca roy o 346 Ar 176 84 130 127 171 120 134 189 Tesuque s 2 Kilometers 145 142 222 asa 2 Miles 15 0 0 171 159 147 159 Geologic map compilation boundary 1 149 88 145 e 0 155 171 145 152 165 175 98 167 176 165 175 u qu Tes Scale 1:200,000 NAD83 160 147 Rio 159 159 147 147 159 243 Tribal Land boundary 159 220 270 141 145 306 489 Ri oG 134 183 317 80 180 175 193 185 Tesuque Pueblo 3960000 ña de Ca 150 206 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic M San arco sA o r r oy 171 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 24–Bicarbonate alkalinity for ground water in the southern Española Basin. 178 276 180 Lamy 160 221 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 225 3930000 570 709 289 403 415 151 309 243 515 931 420000 30 0 270 410000 3950000 246 250 78 92 200 30 0 390000 3 6 410000 8 6 5 7 ña d aA n ch a 10 4 ra n oG Ri 2 3 4 3 4 asa lab 30 6 7 7 5 Sa nt a 9 6 Cieneguilla 7 32 La Cienega Fe ve r 48 Ri 2 4 5 8 10 26 12 8 5 5 1 4 3 0 ga Ciene 16 16 10 16 16 4 19 2 9 4 632 G in all aA 41 26 41 19 6 78 4 5 rro yo 13 29 60 85 21 30 27 18 8 29 19 8 7 18 22 20 31 El Dorado 31 66 60 61 9 38 10 56 8 4 32 47 30 25 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 10 35 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic M San arco sA 10 o 7 r r oy Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 25– Chloride concentration for ground water in the southern Española Basin. 70 20 8 10 27 9 10 Cl isocon NMOSE Piezometers 16 12 5 Cl concentration in mg/L 21 24 Cr eek 27 Chloride (Cl) 59 16 6 eek za C r YLM#3 7 Surface water sample with CI concentration Supply wells B o na n 10 7 61 47 31 do Ho n 2 6 19 9 2 3 2 1 16 11 Well sample with CI concentration 3 2 Santa Fe 86 22 3 2 2 10 oy o Ar r 12 30 60 14 13 Little Tesuq ue Creek 37 46 26 10 10 3 4 6 14 12 5 15 10 9 4 13 11 10 10 7 19 4 13 3 6.4 10 12 15 12 2 40 113 13 11 21 7 14 41 11 4 18 9 0 11 23 37 9 3 Ca roy o Ar Agua Fria 4 10 10 12 4 5 2 3 6 WWTP 20 10 9 2 2 25 2 4 2 3 7 2 YLM#2 s 3 2 14 6 2 1 2 38 13 4 4 2 15 7 4 3 10 Geologic map compilation boundary 4 16 Tesuque 19 2 4 3 4 87 4 4 3 8 10 18 4 5 Tribal Land boundary 5 3 ue 4 5 4 4 3 5 5 4 10 30 60 90 10 q esu oT Ri 4 6 6 3 4 4 5 11 14 5 9 5 2 Kilometers 10 17 25 4 4 7 5 8 Scale 1:200,000 NAD83 0 1 2 Miles 20 6 8 5 9 10 18 Tesuque Pueblo de Ca 6 0 420000 3960000 6 5 3950000 3 115 55 400000 3 3940000 2 2 2 16 10 29 37 12 Lamy 19 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 390000 390000 400000 410000 420000 ND ND ND 0.15 0.11 Tesuque Pueblo 0.11 0.18 ra n de 0.15 0.11 ND 3960000 0.12 Tribal Land boundary 0.1 0.05 ND e ND ND n cha 2 Miles Geologic map compilation boundary 0.1 ND ND ND 0.04 ND asa s ND 0.18 0.14 ND 0.03 0.2 0.23 YLM#2 ND 0.06 ND ND 0.17 ND 0.03 roy o Ar 0.05 Agua Fria ND ND ND 0.3 Santa Fe 0.03 0.2 ND ND Little Tesuq ue Creek 0.12 0.18 ND lab 2 Kilometers ND ND ND Ca 0 ND da A 1 ND u qu Tes C a ña 0 Tesuque Rio ND ND Scale 1:200,000 NAD83 0.02 3950000 Ri oG ND 0.49 0.21 ND ND ND ND WWTP Cieneguilla R Fe r ive ND ND Ciene 0.12 0.02 0.11 0.94 B o na n eek ga Cr eek za C r 0.1 YLM#3 Bromide (Br) lli n Ga aA 0.2 rro yo ND NMOSE Piezometers 0.3 0.17 0.15 0.36 El Dorado 0.79 0.47 0.23 0.8 0.11 0.2 0.1 0.41 0.2 Br isocon Well sample with Br concentration ND = none detected @ 0.1 mg/L Surface water sample with Br concentration Supply wells 0.56 0.27 0.1 0.2 Br concentration 0.3 mg/L 0.4 20 do 0.03 ND La Cienega Ho n oy o Ar r 3940000 Sa nt a 0.2 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic S a an M rcos Ar r oy o Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 26– Bromide concentration for ground water in the southern Española Basin. 0.4 0.3 0.4 0.42 0.2 Lamy 0.19 ND 0.1 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 ND 400000 ---73 47 410000 420000 58 73 Tribal Land boundary Tesuque 69 Rio 10 82 e 51 52 YLM#2 52 30 13 60 178 141 90 Ar roy o 101 30 106 Agua Fria -27 44 nt r ive eR aF Ho n oy o Ar r 30 do 60 3940000 Sa 123 ---- WWTP 62 Cieneguilla ga Ciene 66 La Cienega 82 78 672 B o na n Cr eek eek za C r YLM#3 60 G i na all A 10 rro 48 60 47 yo 50 10 20 Well sample with CI:Br ratio Supply wells NMOSE Piezometers 30 50 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic San Ma A rcos r r oy o 10 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) 66 84 60 265 70 30 35 78 10 30 Cl concentration 60 in mg/L 90 50 El Dorado 70 Chloride:Bromide Ratio 60 Cl isocon Santa Fe 1353 lab asa s 58 52 Ca 2 Kilometers 10 63 Geologic map compilation boundary 2 Miles Little Tesuq ue Creek 125 83 -- n cha 0 1 10 da A 0 u qu Tes C a ña Scale 1:200,000 NAD83 94 3960000 10 Ri oG 54 47 -- 3950000 ra n de Tesuque Pueblo 88 Lamy Fault, certain Fault, approximate Fault, concealed Syncline, concealed Figure 27–Ratio of chloride to bromide concentration (mg/L) and chloride concentration contours for ground water in the southern Española Basin. 3930000 390000 20 21 Ca 29 19 ña da A ha ra n Ri oG 27 33 48 29 21 20 21.6 18 27 17 27 29 14 16 12 18.3 13 18.3 La Cienega 57 39 60 Sulfate (S04) YLM#2 21.4 9.4 8.4 asa 4 5.6 12 18 7.1 4.6 4 4.8 5.7 13 12 11 61 25 8.5 11 Little Tesuq ue Creek 15 11 5.1 22.3 13 16.3 17 5 11 15.8 37 22 Santa Fe 17 39.2 30.7 107 100 29 27 12.4 0 4 0 1 43.4 23.6 27 48.1 39 3.6 Agua Fria 12.7 1614 63.2 21 93.6 37.5 51 28 14 3 7.1 0 22 12 25 1112 0 32 0 22 0 14.9 10.2 10 23 33 36 4.3 75.3 0 13 100120 37.8 55.3 WWTP 8 10.2 0 9.9 29 0 51.8 75.3 10.5 7.1 9.3 vi e r54 44 R 16.4 64.2 84 Fe 6.4 19 60 28.9 7 o nd o nt a H a S 12 oy o Ar r 110 4 100 11 7 12.2 7.6 10 34 11 60 16.2 0 15 6.62 16.7 13 14 45 8.9 7 11.4 17.1 eek 8.2 28 ga Cr 62.3 Ciene 22.5 17.1 17 16.4 19.4 17 20 15 k ee r C 18 90 14.5 Bonanza 25 14 17 34 14 33 16 92 13 768 50 38 27 16 59.2 61 yo 31 34 rro 101 72 A 21 37 43 a 16 15 15 la li n 22 El Dorado YLM#3 G 23 16 19 113 16 108 28 0 0 14 9.7 1 60 20 60 S04 concentration in mg/L 100 9.6 6.2 8.9 60 17.6 20 470 100 42 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 60 25 77 170 1 00 56 1560 20 S04 isocon Surface water sample with S04 concentration Supply well NMOSE Piezometer 15 7.1 10 12 7.5 Ca Cieneguilla Well sample with S04 concentration 17 s 19 8.4 roy o 14 14 8.3 15.1 Ar 20 20 16 8.3 Tesuque 11 20.8 7.5 13 lab Geologic map compilation boundary 15 18 13 13.7 9 8.6 20 15 20 18.5 17 3.5 22 27 2 Kilometers 17 18 16 0 22.6 13 e 32 29 29 37.5 u qu Tes 49 40 26 16.6 Tribal Land boundary Rio 0 20 22 55.3 58 18 18 18 2 Miles 29 66 42,46,81 10 29 18 Scale 1:200,000 NAD83 1 Tesuque Pueblo 20 20 42 45 de nc 29 0 0 11.3 20 16 24 420000 3960000 25 23 410000 3950000 12.5 24 28 49 400000 26 54.6 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic San rco Ma sA r r oy o 28 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 28– Sulfate concentration for ground water in the southern Española Basin. 24 197 Lamy 49.9 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 35 3940000 12.3 3930000 11 3 3 20 390000 390000 400000 ad aA nc ha ra n 3 6 5 4 Ri oG 3 3 3 4 2 3 5 4 5 4 4 2 1 4 2 1 2 YLM#2 6 4 1 5 asa s 4 7 1 roy o Ca 3 Ar 2 1 1 1 2 1 n Sa ta R Fe 2 3 La Cienega 1 7 2 4 2 3 3 1 1 2 1 1 2 1 6 0 4 7 1 6 6.5 3 4 3 1 1 1 1 1 2 6 5 1 Ciene Ho n 2 3 2 3 1 a lli n Ga A 1 2 4 rro yo S04: Cl ratio 6 S04: Cl ratio isocon 20 Well sample with S04: Cl ratio Surface water sample with S04: Cl ratio Supply wells NMOSE Piezometers 4 1 1 1 1 3 Cr eek o na nz a YLM#3 1 1 1 3 1 1 2 12 1 1 2 11 1 El Dorado 1 1 3 2 6 1 1 9 25 1 1 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 2 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic S a an M rcos Ar r oy o 3 4 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) 1 0 11 2 3 2 2 4 6 1 2 do 3 S04: Cl Ratio 1 1 0 3 eek ga Cr 3 2 2 1 2 1 0.9 2 1 2 B Santa Fe 0 0 3 3 3 11 11 1 Little Tesuq ue Creek 1 0 00 0 01 0 0 1 1 1 1 oy o Ar r 2 21 1 1 1 3 2 1 0 5 1 0 0 2 1 01 2 2 1 0 1 1 1 1 1 3 0 3 1 2 1 Cieneguilla 4 r ive 5 3 2 2 WWTP 1 1 1 Agua Fria 1 2 2 4 1 Tesuque 3 5 5 0 4 9 4 2 3 3 0 3 4 5 5 2 22 1 2 lab 4 Geologic map compilation boundary 2 Kilometers 1 4 4 2 4 e 0 Tribal Land boundary u qu Tes 4 5 5 5 4 4 4 4 2 Miles 1 5 6 4 2 Rio 4 6 5 4 2 2 2 Scale 1:200,000 NAD83 1 0 3 2 6 4 4 0 0 Tesuque Pueblo 3960000 añ 3950000 2 2C 3 3 3940000 3 de 3 4 420000 4 4 1 Lamy 612 2 Fault, certain Fault, approximate Fault, concealed Syncline, concealed Figure 29–Ratio of sulfate (S04) to chloride (Cl) concentration (meq/L) for ground water in the southern Española Basin. 3 3930000 3 410000 2 3 3 2 4 1 1 2 4 1 400000 0 420000 1.2 1.3 0.5 1.2 Ri Geologic map compilation boundary 1.2 6.7 0.1 5.7 3.5 2.6 3 3.7 0.5 Santa 4.2 0 5 3.3 1.8 3.3 5 3.9 3.4 5.3 8.9 7.3 s asa lab Ca roy o 0 Ar Sa nt a R Fe r ive Cieneguilla La Cienega 0 2.2 0.4 0.3 0.6 0.4 Ho n 0.7 2.1 2.7 1.2 5.4 6.9 3.7 do 2.9 1.4 2.4 2 1.8 2.9 1.8 3.9 2.7 0.8 1 0.4 0.8 eek ga Cr Ciene 15 k a Cr ee YLM#3 G A i na all 2.3 rro 1.9 yo 3 1.4 1.5 El Dorado 0.2 15 20 N03 concentration >10 mg/L MCL = 10 mg/L Well sample with N03 concentration Surface water sample with N03 concentration Supply wells NMOSE Piezometers 1.8 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo San Ma rcos oy o Ar r Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 30–Nitrate (as N) concentration for ground water in the southern Española Basin. 1 0 4.9 1.8 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic 4.6 2 1.4 6.1 1.9 1.7 0 2.7 1.6 0.9 1.4 1.4 1.6 0.9 N03 concentration 0 1.8 0.5 0.7 6.3 5-10 mg/L 1.1 3.4 0 0 Nitrate (N03(N)) Fe 2.4 2.2 3.5 6.3 oy o Ar r 0.8 Bonanz 0.03 0.07 0.5 3.3 6.3 7.5 0.3 2.2 3.1 2.1 1.5 0 1.6 2.9 1.5 0.3 3.2 2.7 1.6 0.5 2.4 1.6 0 0.2 2.2 1.11.5 1.9 1.9 0.8 0.3 0.3 2 1.3 0.4 0.3 1.6 0.7 3.6 0.8 Agua Fria 0.7 0 4.6 4.6 0 3.4 0.4 1 0.7 4.4 0.3 1.6 4.5 1.7 0.3 9.8 9.8 7.3 2.2 Little Tesuq ue Creek 0.4 0.9 0.3 8.7 WWTP 2.5 2.1 0 0.4 2.3 0.7 0.4 YLM#2 1.2 2.7 e 0.5 0.2 1.5 1 u qu Tes 2 Kilometers 0.5 0.5 0.3 0 0 n cha 0 2 Miles 3.5 Tesuque 1.4 0.6 4 1.5 0.3 0.6 0.4 0.4 0.3 Rio 1 0.7 3.1 3.2 da A 0 1.5 C a ña Scale 1:200,000 NAD83 0.6 3960000 oG ra n de 0.9 1 1 2.1 5.3 0.8 Tribal Land boundary 3.5 0.9 0.6 1.1 1 1.1 1.5 1.2 0 Tesuque Pueblo 4.4 3950000 3.4 410000 0 3940000 1.3 3.5 Lamy 0.2 0.6 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 390000 390000 400000 410000 0.7 0.5 de ra n oG ha 0.7 Ri 0.7 0.9 1.2 0.6 0.9 0.9 0 0.5 0.5 Geologic map compilation boundary 0.4 0.8 1.5 0.5 0.6 0.6 0.3 0.3 asa Ca 0.2 Ar roy o 0.4 0.3 0.4 0.3 WWTP 0.5 0.2 0 0.6 0 Sa nt a Fe 0.2 0.3 0.2 0.7 0.2 0.2 0.2 0.3 0.3 0.4 0.2 0.2 Santa Fe 0.1 1.4 0.2 0.1 1.6 1.7 0.2 0.2 0.2 0.2 0.2 0.5 0.3 0.5 1 Fin concentration mg/L 2 2 20 F isocon Well sample with F concentration Surface water sample with F concentration Supply wells NMOSE Piezometers 1 YLM#3 G A i na all 1 1 rro 0.5 0.3 yo 1 1.9 0.6 0.9 0.7 0.5 0.4 0.5 1.9 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic 1 0.5 0.9 1.8 0.4 San Ma rcos oy o Ar r Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 31–Fluoride concentration for ground water in the southern Española Basin. 0 1.2 1.5 0.7 0.4 1 1.6 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 1.4 0.5 El Dorado 0.3 0.6 1.8 0.9 0.8 0 0.6 0.6 0.5 0.5 Fluoride (F) 0.4 0.4 0.5 0.5 0.2 0.9 0.6 0.5 0.6 0.5 0.7 0.7 1.2 0.5 0.6 0.1 eek ga Cr Ciene r eek 0.4 Bonanza C 0.7 0.3 0.6 2.1 3.5 2 0.3 0 0.3 0.2 0.2 0.3 0.5 0.4 0.4 0.4 0.1 0.2 0.4 0.2 0.2 0.2 0.2 0 0 0 0.6 0 0 Agua Fria 0.1 2.7 3.6 0.2 0.3 0.3 0.2 0.2 00 0.2 0.3 0.2 0 0.2 0.2 0.2 0.2 0.3 0 0.2 00.2 0 0.2 0.2 do 0.1 Ho n 0 Little Tesuq ue Creek 1 0.2 0.4 0.5 0.3 0.1 0.4 0.2 0.5 1 0.2 0 0.2 0.2 0.3 0.2 0.2 0.4 0 1.2 0.4 0.4 0.3 0.4 oy o Ar r 0.3 0.3 0.2 0.6 0.2 0.5 La Cienega 0.4 0.3 Cieneguilla 0.3 0.3 ve r0.1 Ri 0.4 0.4 0.5 0.4 2 1.6 0.3 0.2 0.4 s 0.3 0.3 0.2 Tesuque 0.3 0.3 0.4 0 0.3 0.3 YLM#2 0.4 0.2 0.3 0.3 0.2 0.2 0.3 0.3 0.3 lab 2 Kilometers 0.4 0.2 0.2 1.8 1 0.5 0.5 0.5 0.4 0.3 0.3 1.9 0.3 e 0 0.7 0.4 0.2 u qu Tes 0.7 0.6 0.5 Tribal Land boundary 0.5 Rio 0.4 1 0.5 0.4 Scale 1:200,000 NAD83 2 Miles 0.5 0.3 0.5 0.2 0.3 0.1 1.4 0.5 0.6 0.3 0.9 1 0.3 0.3 0.3,0.3,0.2 3960000 0.3 0.8 0.7 nc Tesuque Pueblo 3950000 aA 3940000 ad 0.5 0.2 C 0.4 0.7 0.5 0.3 0.4 0.9 1.3 0.9 Lamy 0.8 0.8 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 0.4 0.4 0.7 añ 0 420000 0.7 0.3 0.5 0.4 0.4 0.1 0.4 400000 22 2 3 8 10 ND Tesuque Pueblo 5 de ra n 2 8 3 6 Ri oG 4 5 10 14 11 3 11 8 asa Ar 1 1 4 5 10 2 2 ND Ho n ND ND ND ND ND ND 3 do ND ND eek za C r 18 10 B o na n 12 ND YLM#3 4 G i na all ND 2 eek ga Cr Ciene A y rro o ND 5 5 5 3 9 2 2 2 ND El Dorado 1 ND 2 ND ND 5 1 ND ND 2 5 6 Well sample with As concentration 4 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 10 4 5 3 2 20 As isocon None detected Surface water sample with As concentration Supply well NMOSE Piezometer 6 8 2 10 5 9 10 1 ND ND 1 2 4 ND 5 2 11 oy o Ar r 323 34 7 5 10 concentration 20 As in µg/L 30 40 ND 5 ND ND ND 2 3 ND ND 18 5 ND ND ND ND 2 ND ND 4 ND 10 4 Arsenic (As) 20 7 5 5 5 4 Santa Fe ND 1 Ca roy o 1 r ive 3 4 2 5 2 1 ND 5 nt eR aF 5 La Cienega 8 3 WWTP Cieneguilla ND 5 9 Agua Fria 1 Sa 2 3 ND 7 lab 30 3 1 18 42 ND 4 ND Little Tesuq ue Creek 6 5 14 s 40 10 20 4 2 ND 11 9 11 7 YLM#2 14 ND e ND 17 15 14 Tesuque 3 4 16 54 4 3 14 20 ND 3 5 16 16 9 7 10 13 7 u qu Tes Geologic map compilation boundary 12 30 29 5 Tribal Land boundary Rio 2 Kilometers n cha 0 2 Miles 7 4 0 21 da A 1 C a ña 0 5 3 5 ND <20 ND <20 ND <20 18 Scale 1:200,000 NAD83 4 ND 7 ND ND 55 8 4 19 7 6 3960000 4 5 5 7 3950000 6 2 ND 420000 3940000 16 410000 0 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic San M s arco Ar r oy o Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 32– Arsenic concentration for ground water in the southern Española Basin. 2 7 Lamy Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 11 3 5 390000 (A) 0 Depth below water table (feet) 500 1000 1500 MCL = 10 µg/L SF-2 and SF-3,piezometer set B Buckman piezometer D Buckman #10 Buckman #11 Buckman #13 Las Campanas piezometer H 2000 2500 0 5 10 15 20 25 30 35 40 Arsenic (µ g/L) (B) 0 Archery piezometer C Santa Fe River piezometer E Fairgrounds piezometer F 600 900 MCL = 10 µg/L Depth below water table (feet) 300 1200 1500 1800 0 5 10 15 20 25 30 35 40 Arsenic (µ g/L) Figure 33– Variation in arsenic concentration with depth in piezometer nests located near (A) Buckman and (B) Santa Fe. 45 390000 400000 410000 420000 10 5 Tesuque Pueblo >19˚ 5 Ri oG 5 ' 30 0 0 e Geologic map compilation boundary Tesuque >2 <2 u qu Tes 60 0 Little Tesuq ue Creek 0' ' ' Santa Fe YLM#2 asa lab Agua Fria 30 0 0' WWTP 50 10 0 0' 20 0 0' 0' do 5 Ciene B o na n eek ga Cr eek za C r 50 0 ' <19˚ 0' lli n rro yo 5 El Dorado >2 3930000 25 Ga YLM#3 aA 0' 2 Ground water isotherm (Figure 13) Ca:Na ratio isocon (Figure 22) Depth contours (ft) to top of Oligocene volcanics, and Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Bedrock boundary Ho n 25 19° 0' 10 As concentration in µg/L 5 10 5 10 20 30 40 r ive 10 5 oy o Ar r La Cienega >19˚ Arsenic (As) R Fe 3940000 25 Cieneguilla Sa Ca roy o 0' Ar 5 40 0 s 40 30 10 20 nt a 3950000 00 30 0 0 50 20 0 0' 2 Kilometers 0' n cha 0 2 Miles 10 da A 1 C a ña Scale 1:200,000 NAD83, UTM Zone 13 Tribal Land boundary Rio 70 0 0 3960000 ra n de <19˚ 5 <2 >19˚ 25 Surface water sample with As concentration Supply well NMOSE Piezometer 0' San Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ma rcos A <19˚ Lamy o r r oy Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic Fault, certain Fault, approximate Fault, concealed Syncline, concealed Figure 34–Spatial correlation of high arsenic concentration with elevated ground water temperature and sodium concentration. Arsenic Concentration (mg/L) 40 30 20 10 0 0 1 2 3 4 5 6 7 8 9 10 Calcium/Sodium Ratio Figure 35–Plot of arsenic concentration and calcium-to-sodium ratio. All arsenic samples with concentrations above 10 µg/L occur in sodium-rich water with a Ca:Na ratio less than 2. Lower arsenic concentrations occur across a range of cation ratios. fines Feet 0 general grain size sand peb- cobbles vf f m c vc bles Yates La Mesa #2 Tts, Lithosome S of Tesuque Fm sand and gravel 404’ 500 Sand, pebbly sand with major mud/clay interbeds 875’ 1000 Sand and pebbly sand with minor mud/clay interbeds 1459’ 1500 Muddy sand with higher gamma ray 2000 2261’ Sand with 10-50% mudstone 2500 2475’ Mud (10-90%) with sand interbeds 2705’ 3000 Brick red shales and very fine sandstone; correlates (?) to seismic reflector. 3500 Transition zone to higher gamma, volcaniclastic sediments Tte, Lithosome E of Tesuque Fm Greenish volcaniclastic sandstone with minor mudstone 3580’ 3715’ 4000 3862’ 3900’ Muddy basaltic sand with mud bed at top TI, TERTIARY INTRUSIVE 4292’ 4336’ 4428’ 4500 5000 potential source rocks 5013’ for arsenic in groundwater Highgamma ray intermediate sill Tci, Cieneguilla Basanite Basalt flow and sill 4664’ Mafic volcaniclastic 4740’ 4812’ Ash, high gamma-ray and thorium Basalt, with arkosic, volcaniclastic sediment 5071’ Te, Espinosa Fm Latitic volcaniclastic sediment 5500 5584’ 5710’ Intermediate volcanic sill Volcaniclastic and arkosic sediment 6000 5945’ 6020’ Paleozoic Rocks Pa, Permian Abo or &m, Pennsylvanian Madera Fm. 6500 Stratigraphic unit boundaries from D. Koning & D. Sawyer, personal communication Figure 36–Generalized stratigraphic column for Yates La Mesa #2, showing potential source rocks for arsenic in ground water west of Santa Fe. 400000 100 163 200 250 400 200 Tesuque Pueblo 15 0 140 Tribal Land boundary 86 300 99 Geologic map compilation boundary 230 180 180 170 160 150 100 130 YLM#2 s asa 650 13 170 230 410 860 860 340 400 380 800 845 258 250 500 300 200 50 0 556 200 400 620 535 240 170 120 lab Ca Agua Fria 200 150 195 72 200 200 100 300 150 160 YLM#3 Supply wells NMOSE Piezometers Cr eek G in all aA 390 80 rro yo 40 48 98 61 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo 110 160 47 El Dorado 77 90 150 80 76 14 200 Ba isocon Surface water sample with Ba concentration 0 25 134 80 Well sample with Ba concentration 100 200 159 150 concentration 250 Ba in µg/L 500 20 do eek ga Cr Ciene 99 Barium (Ba) Ho n 60 117 190 120 Bonanza 15 6 80 170 220 250 15 0 110 72 160 190 oy o Ar r 120 49 200 300 ve r Ri 100 La Cienega 130 200 55 Cieneguilla 180 15 0 roy o Ar 150 100 110 100 WWTP Fe Santa Fe 140 170 110 29 nt a Little Tesuq ue Creek 280 230 160 110 190 Sa 6 120 23 110 55 160 e 200 120 88 110 80 130 u qu Tes 2 Kilometers Rio 0 2 Miles Tesuque 150 170 103 150 113 110 160 n cha 1 160 150 130 da A 0 110 100 C a ña Scale 1:200,000 NAD83 3960000 de oG ra n 34 120 89 Ri 100 87 110 130 210 3950000 200 420000 3940000 100 100 410000 Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic 2 200 150 6 70 San Ma rcos A o r r oy Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 37– Barium concentration for ground water in the southern Española Basin. 40 65 50 68 Lamy 16 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 14 1 16 34 75 15 0 390000 390000 400000 346 420 de ra n oG Ri 652 300 150 290 120 e 96 Geologic map compilation boundary 260 170 190 160 222 380 300 Ca lab asa s 270 270 roy o Ar Sa nt a Fe 300 350 250 190 290 420 74 100 110 87 180 150 360 do 170 220 Cr eek ga Ciene 160 Bonanza 47 La Cienega Ho n oy o Ar r 210 Cr eek 810 YLM#3 330 G i na all A rro 290 yo 290 Strontium (Sr) 280 El Dorado 440 280 0 45 150 720 600 240 200 340 470 150 Sr isocon NMOSE Piezometers 120 410 90 150 300 Sr concentration 450 in µg/L 600 Well sample with Sr concentration Surface water sample with Sr concentration Supply wells 0 45 530 440 300 20 230 130 240 230 110 130 Santa Fe 110 150 ve r Ri 160 240 67 Agua Fria 83 200 49 Cieneguilla 360 300 YLM#2 340 270 Little Tesuq ue Creek 130 310 530 WWTP Tesuque u qu Tes 2 Kilometers 250 Rio 440 n cha 2 Miles 450 Tribal Land boundary 424 da A 0 300 610 320 C a ña 1 450 620 180 243 Scale 1:200,000 NAD83 480 450 300 304 0 750 600 760 580 3960000 450 Tesuque Pueblo 3950000 824 420000 3940000 600 410000 350 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic S a an M rcos Ar r oy o 300 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 38–Strontium concentration for ground water in the southern Española Basin. Lamy Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 290 10 67 150 390000 400000 6 12 9 6 añ ad n ch a 12 ra n Geologic map compilation boundary 4 1 2 3 5 3 0 YLM#2 3 0 2 1 3 2 1 0 0 0 0 0 0 0 1 0 0 Santa Fe 2 lab asa s 4 2 3 roy o 1 1 Ar 2 2 1 11 Agua Fria 0 5 7 3 2 4 2 6 WWTP Cieneguilla n Sa ta R Fe r ive Ho n oy o Ar r 2 do 3940000 4 Little Tesuq ue Creek 2 6 8 9 4 2 1 3 ga Ciene La Cienega 8 4 3 3 2 13 5 10 2 3 Ca 2 Kilometers 5 5 2 5 6 Tesuque 3 e 0 2 Miles 9 u qu Tes 1 Tribal Land boundary 4 Rio Scale 1:200,000 NAD83 51 8 ND <100 ND <100 ND <100 ND <100 ND <100 0 ND <100 ND <100 8 ND <100 ND <100 ND <100 ND <100 0 0 13 ND <100 ND <100 ND <100 Ri oG 8 Tesuque Pueblo 10 8 5 de 10 aA 3960000 16C 3950000 10 2 2 0.7 B o na n Cr eek eek za C r 21 9 4 YLM#3 3 G in all aA rro 2 yo 2 3 2 2 8 3 4 16 El Dorado 3 3 2 2 3 10 4 5 10 3 U concentration in µg/L 10 U isocon 20 Well sample with U concentration Surface water sample with U concentration Supply well NMOSE Piezometer 19 6 Uranium (U) 2 Qta, Ancha Tt, Tesuque Te, Espinaso Tg, Galisteo Ti, Intrusives Precambrian bedrock Mesozoic and Paleozoic San rco Ma sA r r oy o 5 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 39– Uranium concentration for ground water in the southern Española Basin. 0 3 32 Lamy 10 Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 116 420000 10 15 410000 5 28 3 1 9 22 -50 Local Metoric Water Line, δD = 8.0 d18O + 11.1 (Anderholm 1994) Deuterium-enriched ground water Mixed groundwater Deuterium-depleted ground water -60 Surface Water (Anderholm 1994) Rio Grande at Otowi (Mills 2003) Santa Fe River Little Tesuque Creek Tesuque Creek Rio Tesuque Rio Pojoaque Arroyo Hondo Rio Chupadero δ2H ‰ -70 -80 -90 Mixed D-Depleted ? -100 Deuterium-depleted Groundwater -110 -120 -17 -16 -15 -14 -13 -12 -11 -10 -9 δ O‰ 18 Figure 40–Values of δ2Η and δ18O isotopic composition for all ground water and surface water samples from the southern Española Basin in relation to the local meteoric water line of Anderholm (1994) -8 390000 400000 -105 -85 -111 -96 -89 Ri -78 Tribal Land boundary -117 Geologic map compilation boundary -88 -97 -89 s asa lab Ca roy o WWTP Sa nt ve r Ri -81 -77 -100 -80 -83 La Cienega -83 -77 -75 -81 -79 -81 Ciene B o na n YLM#3 -78 -76 -77 -7 0 -61 -85 -66 on do -78 -68 -76 -73 -73 -72 -79 -82 -73 eek za C r -8 0 Ga lli n aA rr oy o -71 -93 -77 -93 -73 -72 El Dorado -82 -7 0 -66 -8 0 -94 -82 -73 -98 -75 Supply wells NMOSE Piezometers Exploration well San rco Ma sA r r oy o Lamy -9 0 -70 δ ²H ratio isocon Well sample with δ ²H value -71 -9 0 -70 -80 units = ‰, parts -90 per thousand -100 -77 -79 -81 δ ²H Composition 20 -74 eek ga Cr -94 -77 δ ²H <-100 ‰ Deuterium depleted -80 Santa Fe -75 H Ar royo -77 -9 0 Little Tesuq ue Creek -78 -92 -73 -80 -79 -77 -80 -74 -76 -83 -68 -80 Agua Fria -77 -78 -75 -81 -80 -79 -82 -67 -78 -80 -80 -80 Ar -94 -72 -77 -80 -83 e aF -8 -72 0 -83 YLM#2 -113 -104 -87 -82 -85 -93 -89 -85 -84 -79 -9 0 -93 -9 0 e -88 -112 -114 -82 -82 -81 -80 -87 -85 -85 -86 -85 u qu Tes 2 Kilometers -84 -99 n cha 0 2 Miles -82 -85 da A 1 -94 -97 C a ña 0 Rio -98 -77 Tesuque -99 3960000 oG -116 -74 -108 -92 -101 -103 3950000 de -110 -104 ra n -107 -9 0 -9 0 -1 00 Tesuque Pueblo 3940000 -1 0 0 -85 Scale 1:200,000 NAD83 420000 -8 0 -117 -112 410000 Bedrock boundary Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) Figure 41– Stable hydrogen isotopic composition, δ ²H, for ground water in the southern Española Basin. Fault, certain Fault, approximate Fault, concealed Syncline, concealed 3930000 -77 -87 -87 - 92 (A) 0 Depth below water table (feet) 500 1000 Modern Deuterium-depleted 1500 SF-2 and SF-3 piezometer B Buckman piezometer D Las Campanas piezometer H Leyba domestic wells 2000 2500 -120 -110 -100 -90 -80 -70 δ H (per mil ‰) 2 (B) 0 Santa Fe river piezometer E Archery piezometer C Fairgrounds piezometer F Jail piezometer G Depth below water table (feet) 300 600 Modern 900 Deuterium-depleted 1200 1500 1800 -120 -110 -100 -90 -80 -70 δ H (per mil ‰) 2 Figure 42–Variation in stable hydrogen, δ 2Η, composition with depth in multiple completion piezometer nests near (A) Buckman and (B) Santa Fe. Fau lt lt CK RO D BE R FE UI Q A 3930000 0' R io G ra n de CERRIL L OS UPL IF T F au YLM#3 E 0' a ge R ' 00 50 5 Kilometers 5 Miles 25 4 U 3 25 A F E P L A T F O R M 0' X 2 E Scale 1:200,000 T lt V ill 0' 25 0' N ' au 3940000 on Se t 50 A FL 50 0 25 S 3960000 do l ed N 0 1 BE D ROCK rF B L O C K Ho n ea E 0 er Fe nc C Riv Fe a t Sa n n ta co O E La Cienega Sa e R iv 3950000 ' 30 00 Geologic map compilation boundary F R O N T Santa Fe M O U N T A I N ' e, IG 0' 420000 e U N T A I N M O e lin L 20 0 0' uqu nc O 10 0 id ro S an Is ' Sy 30 00 30 00 Z O N EC ro s sin g Fa ult YLM#2 ' 40 00 STRUCTURE 0' N S I B A Depth contours (ft) to top of Oligocene volcanics, and Limits of Cerros del Rio volcanic field. (Grauch and Bankey 2003) 60 0 0' a mb Tesuque Pueblo AS Gradient in domestic well pair Downward Upward Neutral Las Dos Fau lt 70 0 Te s t a ul nF L R A N T C E ma Downward hydraulic gradient Upward hydraulic gradient ANC uck Supply well Piezometer Rio st B RR lt a Fa u BA Ja c o n We Aquifer Domains Ri o N 410000 Az te c S y n Sc p r in g s line 400000 20 00 ' 390000 NT TE E X Figure 43– Aquifer compartmentalization and ground water flow domains in the Tesuque Aquifer System. as e r it o Tij onc lt ñ u Ca F a