630:
708:
694:
394:
286:
723:
637:
743:
733:
602:, who studied the Neogene uplift of the Eastern Andes in Colombia, defines the main stage of uplift between six and four million years ago. Other Dutch geologists Helmens, Van der Hammen and Hooghiemstra have pushed back this uplift phase to between 4.5 and 3 Ma. The upper part of the Tilatá Formation is time-equivalent with the
474:, from approximately 5.3 to 2.7 Ma), and has a maximum thickness of 83 metres (272 ft). The formation underlies the Quaternary sequence of alluvial, lacustrine and fluvial sediments of
1132:
1092:
1087:
1077:
531:
The Tilatá Formation is the lowermost of the lacustrine and alluvial sequence of the Bogotá savanna. It unconformably overlies the
Cretaceous
629:
1127:
1117:
1054:
346:
226:
1137:
615:
471:
436:
269:
1112:
339:
219:
1122:
860:
Monsalve, Maria Luisa; Rojas, Nadia R.; Velandia P., Francisco A.; Pintor, Iraida; Martínez, Lina
Fernanda (2011),
1082:
645:
746:
722:
432:
265:
726:
559:
475:
655:
381:
1107:
1102:
516:
447:
193:
599:
563:
671:
659:
555:
491:
144:
126:
742:
732:
314:
544:
424:
166:
586:, with reported ages between 5.3 and 2.7 Ma. The depositional environment has been interpreted as
570:; Tequendama, Tibagota (Lower Tilatá) and Guasca (Upper Tilatá). The age has been estimated to be
603:
548:
170:
1020:
999:
974:
953:
932:
907:
736:
840:
Molnar, Peter (2004), "Late
Cenozoic increase in accumulation rates of terrestrial sediment",
594:, formed during the main phase of tectonic uplift of the Eastern Ranges in the Late Pliocene.
536:
428:
261:
158:
849:
567:
412:
853:
1097:
699:
540:
532:
486:
The formation was first defined and named by
Scheibe in 1933 after the Hacienda Tilatá in
162:
154:
667:
995:
928:
861:
713:
587:
1071:
1048:
579:
463:
76:
32:
24:
707:
591:
663:
595:
487:
324:
51:
1026:
1005:
980:
959:
938:
913:
891:
689:
611:
583:
552:
96:
61:
361:
348:
241:
228:
649:
Type locality of the Tilatá Formation on the northeasternmost Bogotá savanna
512:
451:
197:
101:
45:
675:
862:"Caracterización geológica del cuerpo volcánico de Iza, Boyacá - Colombia"
575:
459:
440:
399:
291:
91:
86:
71:
66:
56:
28:
607:
571:
455:
106:
81:
467:
36:
1050:
Plancha 5-09 del Atlas Geológico de
Colombia 2015 – escala 1:500,000
886:
Montoya Arenas, Diana María; Reyes Torres, Germán
Alfonso (2005),
679:
520:
443:
273:
207:
973:
Ulloa, Carlos E; Rodríguez, Erasmo; Acosta, Jorge E. (1998),
511:
The Tilatá Formation consists of medium to coarse grained
1047:
Gómez, J.; Montes, N.E.; Nivia, Á.; Diederix, H. (2015),
833:
Geología e
Hidrogeología de Santafé de Bogotá y su Sabana
1001:
Plancha 228 - Santafé de Bogotá Noreste - 1:100,000
387:
377:
338:
330:
320:
310:
302:
297:
279:
257:
218:
213:
203:
189:
184:
176:
150:
140:
132:
122:
18:
835:, Sociedad Colombiana de Ingenieros, pp. 1–20
446:. The formation consists of coarse to very coarse
769:
767:
765:
763:
761:
614:and the main phase of explosive activity of the
994:Buitrago, José Alberto; Terraza M., Roberto;
842:Annual Review of Earth and Planetary Sciences
8:
952:Montoya, Diana María; Reyes, Germán (2009),
906:Renzoni, Giancarlo; Rosas, Humberto (2009),
1019:Acosta, Jorge E.; Ulloa, Carlos E. (1998),
566:(1995) subdivided the formation into three
15:
831:Guerrero Uscátegui, Alberto Lobo (1992),
527:Stratigraphy and depositional environment
636:
136:Tequendama Mb., Tibagota Mb., Guasca Mb.
757:
747:Geology of the Altiplano Cundiboyacense
854:10.1146/annurev.earth.32.091003.143456
927:Renzoni, Giancarlo; Rosas, Humberto;
654:The Tilatá Formation is found at its
7:
1133:Geography of Cundinamarca Department
1022:Plancha 246 - Fusagasugá - 1:100,000
454:. The Tilatá Formation dates to the
955:Plancha 209 - Zipaquirá - 1:100,000
14:
976:Plancha 227 - La Mesa - 1:100,000
909:Plancha 171 - Duitama - 1:100,000
618:, active between 4.7 and 3.6 Ma.
1093:Pliocene Series of South America
741:
731:
721:
706:
692:
635:
628:
392:
284:
1088:Miocene Series of South America
1078:Geologic formations of Colombia
934:Plancha 191 - Tunja - 1:100,000
888:Geología de la Sabana de Bogotá
791:Montoya & Reyes, 2005, p.67
782:Montoya & Reyes, 2005, p.69
773:Montoya & Reyes, 2005, p.68
1:
1055:Servicio Geológico Colombiano
818:Guerrero Uscátegui, 1992, p.6
494:. Hubach (1957) elevated the
180:up to 83 m (272 ft)
809:Monsalve et al., 2011, p.120
727:Geology of the Eastern Hills
737:Geology of the Ocetá Páramo
1154:
616:Paipa–Iza volcanic complex
551:, and is overlain by the
23:
1128:Altiplano Cundiboyacense
658:in the synclinal of the
433:Altiplano Cundiboyacense
266:Altiplano Cundiboyacense
1118:Conglomerate formations
670:valley, and along the
460:Early to Late Pliocene
416:
362:5.099139°N 73.713806°W
242:5.099139°N 73.713806°W
929:Etayo Serna, Fernando
1113:Sandstone formations
646:class=notpageimage|
556:Subachoque Formation
472:SALMA classification
425:geological formation
367:5.099139; -73.713806
247:5.099139; -73.713806
145:Subachoque Formation
127:Geological formation
1138:Geography of Bogotá
869:Boletín de Geología
600:Salomon Kroonenberg
549:Regadera Formations
358: /
238: /
29:Early-Late Pliocene
25:Stratigraphic range
800:Molnar, 2004, p.75
604:Chorrera Formation
535:and the Paleogene
1123:Alluvial deposits
405:
404:
1145:
1083:Neogene Colombia
1064:
1063:
1062:
1036:
1035:
1034:
1015:
1014:
1013:
990:
989:
988:
969:
968:
967:
948:
947:
946:
923:
922:
921:
895:
894:, pp. 1–104
882:
881:
880:
866:
856:
836:
819:
816:
810:
807:
801:
798:
792:
789:
783:
780:
774:
771:
745:
735:
725:
716:
711:
710:
702:
697:
696:
695:
639:
638:
632:
498:to a formation.
417:Formación Tilatá
409:Tilatá Formation
398:
396:
395:
373:
372:
370:
369:
368:
363:
359:
356:
355:
354:
351:
290:
288:
287:
253:
252:
250:
249:
248:
243:
239:
236:
235:
234:
231:
118:
48:
19:Tilatá Formation
16:
1153:
1152:
1148:
1147:
1146:
1144:
1143:
1142:
1068:
1067:
1060:
1058:
1046:
1043:
1032:
1030:
1018:
1011:
1009:
996:Etayo, Fernando
993:
986:
984:
972:
965:
963:
951:
944:
942:
926:
919:
917:
905:
902:
885:
878:
876:
864:
859:
839:
830:
827:
822:
817:
813:
808:
804:
799:
795:
790:
786:
781:
777:
772:
759:
755:
712:
705:
700:Colombia portal
698:
693:
691:
688:
660:Sisga Reservoir
652:
651:
650:
648:
642:
641:
640:
624:
588:alluvial plains
533:Guadalupe Group
529:
509:
504:
496:Pisos de Tilatá
492:Sisga Reservoir
484:
422:
393:
391:
366:
364:
360:
357:
352:
349:
347:
345:
344:
306:Hacienta Tilatá
285:
283:
268:
246:
244:
240:
237:
232:
229:
227:
225:
224:
157:
117:
116:
115:
114:
109:
104:
99:
94:
89:
84:
79:
74:
69:
64:
59:
54:
43:
42:
40:
12:
11:
5:
1151:
1149:
1141:
1140:
1135:
1130:
1125:
1120:
1115:
1110:
1105:
1100:
1095:
1090:
1085:
1080:
1070:
1069:
1066:
1065:
1042:
1041:External links
1039:
1038:
1037:
1016:
991:
970:
949:
924:
901:
898:
897:
896:
883:
857:
837:
826:
823:
821:
820:
811:
802:
793:
784:
775:
756:
754:
751:
750:
749:
739:
729:
718:
717:
714:Geology portal
703:
687:
684:
644:
643:
634:
633:
627:
626:
625:
623:
620:
564:Van der Hammen
562:. Helmens and
528:
525:
508:
505:
503:
500:
483:
480:
437:Eastern Ranges
429:Bogotá savanna
420:
403:
402:
389:
385:
384:
379:
375:
374:
342:
336:
335:
332:
328:
327:
322:
318:
317:
312:
308:
307:
304:
300:
299:
295:
294:
281:
277:
276:
270:Eastern Ranges
262:Bogotá savanna
259:
255:
254:
222:
216:
215:
211:
210:
205:
201:
200:
191:
187:
186:
182:
181:
178:
174:
173:
152:
148:
147:
142:
138:
137:
134:
130:
129:
124:
120:
119:
112:
111:
110:
105:
100:
95:
90:
85:
80:
75:
70:
65:
60:
55:
50:
49:
21:
20:
13:
10:
9:
6:
4:
3:
2:
1150:
1139:
1136:
1134:
1131:
1129:
1126:
1124:
1121:
1119:
1116:
1114:
1111:
1109:
1108:Montehermosan
1106:
1104:
1103:Chapadmalalan
1101:
1099:
1096:
1094:
1091:
1089:
1086:
1084:
1081:
1079:
1076:
1075:
1073:
1056:
1052:
1051:
1045:
1044:
1040:
1028:
1024:
1023:
1017:
1007:
1003:
1002:
997:
992:
982:
978:
977:
971:
961:
957:
956:
950:
940:
936:
935:
930:
925:
915:
911:
910:
904:
903:
899:
893:
889:
884:
874:
870:
863:
858:
855:
851:
847:
843:
838:
834:
829:
828:
824:
815:
812:
806:
803:
797:
794:
788:
785:
779:
776:
770:
768:
766:
764:
762:
758:
752:
748:
744:
740:
738:
734:
730:
728:
724:
720:
719:
715:
709:
704:
701:
690:
685:
683:
681:
677:
673:
669:
665:
661:
657:
656:type locality
647:
631:
621:
619:
617:
613:
609:
605:
601:
597:
593:
592:alluvial fans
589:
585:
582:analysis and
581:
580:fission track
577:
576:Late Pliocene
573:
569:
565:
561:
560:Lake Humboldt
557:
554:
550:
546:
542:
538:
534:
526:
524:
522:
518:
517:conglomerates
514:
506:
501:
499:
497:
493:
489:
481:
479:
477:
476:Lake Humboldt
473:
469:
465:
464:Montehermosan
461:
457:
453:
449:
448:conglomerates
445:
442:
438:
434:
430:
426:
418:
414:
410:
401:
390:
386:
383:
380:
376:
371:
343:
341:
337:
333:
329:
326:
323:
319:
316:
313:
309:
305:
301:
296:
293:
282:
278:
275:
271:
267:
263:
260:
256:
251:
223:
221:
217:
212:
209:
206:
202:
199:
195:
192:
188:
183:
179:
175:
172:
168:
164:
160:
156:
155:Guadalupe Gp.
153:
149:
146:
143:
139:
135:
131:
128:
125:
121:
108:
103:
98:
93:
88:
83:
78:
73:
68:
63:
58:
53:
47:
44:5.3–2.7
38:
34:
33:Montehermosan
30:
26:
22:
17:
1059:, retrieved
1049:
1031:, retrieved
1021:
1010:, retrieved
1000:
985:, retrieved
975:
964:, retrieved
954:
943:, retrieved
933:
918:, retrieved
908:
887:
877:, retrieved
872:
868:
845:
841:
832:
825:Bibliography
814:
805:
796:
787:
778:
668:Bogotá River
653:
572:Late Miocene
530:
510:
495:
485:
423:, Tpt) is a
408:
406:
382:Cundinamarca
353:73°42′49.7″W
331:Year defined
298:Type section
233:73°42′49.7″W
194:Conglomerate
171:Regadera Fm.
1057:, p. 1
1029:, p. 1
1008:, p. 1
983:, p. 1
962:, p. 1
941:, p. 1
916:, p. 1
608:outcropping
519:with minor
507:Lithologies
502:Description
490:, near the
365: /
350:5°05′56.9″N
340:Coordinates
245: /
230:5°05′56.9″N
220:Coordinates
159:Guaduas Fm.
1072:Categories
1061:2017-03-16
1033:2017-06-06
1027:INGEOMINAS
1012:2017-06-06
1006:INGEOMINAS
987:2017-06-06
981:INGEOMINAS
966:2017-06-06
960:INGEOMINAS
945:2017-06-06
939:INGEOMINAS
920:2017-06-06
914:INGEOMINAS
892:INGEOMINAS
879:2017-02-25
753:References
612:Subachoque
598:geologist
584:palynology
553:Quaternary
513:sandstones
452:sandstones
167:Bogotá Fm.
875:: 117–130
848:: 67–89,
666:, in the
578:based on
482:Etymology
441:Colombian
303:Named for
198:sandstone
185:Lithology
177:Thickness
163:Cacho Fm.
141:Underlies
133:Sub-units
998:(1998),
931:(1998),
686:See also
664:Chocontá
622:Outcrops
488:Chocontá
458:period;
400:Colombia
325:Chocontá
321:Location
311:Named by
292:Colombia
214:Location
151:Overlies
568:members
537:Guaduas
470:in the
462:epoch (
456:Neogene
439:of the
427:of the
413:Spanish
388:Country
315:Scheibe
280:Country
190:Primary
113:↓
1098:Uquian
676:Bogotá
547:, and
545:Bogotá
523:beds.
468:Uquian
397:
378:Region
289:
258:Region
37:Uquian
865:(PDF)
680:Tunja
674:from
596:Dutch
541:Cacho
521:shale
444:Andes
274:Andes
208:Shale
204:Other
900:Maps
672:road
590:and
515:and
450:and
407:The
334:1933
123:Type
52:PreꞒ
850:doi
678:to
662:in
610:in
574:to
558:of
466:to
419:, N
1074::
1053:,
1025:,
1004:,
979:,
958:,
937:,
912:,
890:,
873:33
871:,
867:,
846:32
844:,
760:^
682:.
606:,
543:,
539:,
478:.
435:,
431:,
421:1t
415::
272:,
264:,
196:,
169:,
165:,
161:,
102:Pg
46:Ma
27::
852::
411:(
107:N
97:K
92:J
87:T
82:P
77:C
72:D
67:S
62:O
57:Ꞓ
41:~
39:)
35:-
31:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.