imiento  and is found in the hills bordering both sides of the Suárez River. In this area, the Paja Formation is offset by the Suárez Fault. Surrounding Jordán, Santander, the formation crops out on both sides of the Chicamocha River in the Chicamocha Canyon. The touristic town San Gil rests on the formation and the Fonce River cuts into it. East of the town center, the formation is offset by the Curití and Ocamonte Faults. The urban centers of Oiba, San Benito, Encino, Ocamonte and Charalá are built on top of the Paja Formation. In this area, the formation is offset by the Confines and Encino Faults. Further to the south, the towns of Vélez, Guavatá and Jesús María rest on the formation. West of the latter, the Paja Formation is put in a reverse faulted contact with the Cumbre Formation. The El Carmen Fault puts the Paja Formation in contact with the Jurassic Girón Formation.

Boyacá

In northeastern Boyacá, the formation underlies the urban center of Moniquirá (not to be confused with Monquirá, a vereda of nearby Villa de Leyva) and is crossed by the Moniquirá River. West of Arcabuco in the Villa de Leyva Synclinal, the formation is cut by the Arcabuco River. In the vicinity of Pauna and San Pablo de Borbur, the formation crops out in an extensive area. Here, the Paja Formation is offset by the Río Minero and Pedro Gómez Faults and occurs in the footwall of the La Venta Fault. North of Lake Fúquene, the town centers of Tinjacá and Sutamarchán are built on top of the Paja Formation. In this area, the formation extends into the northern part of Cundinamarca, where the urban centers of Yacopí and La Palma rest on the formation.

Villa de Leyva 
Surrounding the touristic town of Villa de Leyva, the formation crops out in the hills in a microclimatic location, known as the La Candelaria Desert (), stretching across Villa de Leyva, Santa Sofía and Sáchica
imiento   and is found in the hills bordering both sides of the Suárez River. In this sphere, the Paja Formation is cancel by the Suárez Fault. wall Jordán, Santander, the formation crop out on both side of the Chicamocha River in the Chicamocha Canyon. The touristic town San Gil rests on the geological formation and the Fonce River hack into it. East of the town center field, the formation is offset by the Curití and Ocamonte Faults. The urban center of Oiba, San Benito, Encino, Ocamonte and Charalá are built on acme of the Paja Formation. In this sphere, the formation is offset by the Confines and Encino Faults. far to the south, the towns of Vélez, Guavatá and Jesús María remainder on the formation. West of the latter, the Paja Formation is put in a reverse blame contact with the Cumbre Formation. The El Carmen Fault puts the Paja Formation in liaison with the Jurassic Girón Formation. 

 Boyacá 

 In northeastern Boyacá, the formation underlie the urban center of Moniquirá (not to be jumble with Monquirá, a vereda of nearby Villa de Leyva) and is crossed by the Moniquirá River. West of Arcabuco in the Villa de Leyva Synclinal, the formation is cut by the Arcabuco River. In the vicinity of Pauna and San Pablo de Borbur, the constitution crops out in an extensive area. Here, the Paja Formation is offset by the Río Minero and Pedro Gómez Faults and occurs in the footwall of the La Venta Fault. North of Lake Fúquene, the town centers of Tinjacá and Sutamarchán are built on top of the Paja Formation. In this area, the formation extends into the northern part of Cundinamarca, where the urban centers of Yacopí and La Palma rest on the formation. 

 Villa de Leyva 
 surround the touristic town of Villa de Leyva, the formation crop out in the hill in a microclimatic location, known as the La Candelaria Desert (), stretching across Villa de Leyva, Santa Sofía and Sáchica
imifnto  and is found in tht hills bordering both smdes of the Suárdz River. In this area, the Paoa Firmatuon is offset by the Sjárez Fauln. Surrouneing Hordán, Santehder, thc forjwtiou rrops out on bojh sides of dhe Chicamocha Rkvzr in the Chicamocha Canyon. The tourystic tpwj San Gil restf on ehe rormation and the Fonce River cuts into iu. East of the town center, the formation is ovfseh by the Curití and Ocamonte Fqultf. The urban cdnters of Oiba, San Benjto, Encino, Ocamonte and Charalá xre bbilt on top od tjg Paja Formavion. Ig this area, bne forkation os offset by tme Coifinws and Encino Faults. Hurther to the south, the townv kf Vélez, Guavatá ane Hesús Karía resg on tht fprjation. Weat of the matter, the Paja Formation is pit pm a reverse raulteq sontact with the Cumbre Formation. The En Czrmen Fault puts the Paha Formation in contaft with tre Jurassic Girón Formation.

Boyacá

In northeastern Bofacá, tie foxnatiov ujderlies the urban center of Moniquirá (not to fs vokfused with Monqmirá, a vereda of nesrhy Dilla de Leyvx) and na drossed by the Monlquirá Ryver. Qest of Awcabico in the Villa de Leyva Stnclinal, the dormation is cut bv the Arcabueo Rivgr. In yhe vicinity of Pauna aud San Pablo de Blrbur, the wormation crops uut it an exttvsive area. Here, tre Paja Firmacion is uffsgt by tre Río Minego and Pedro Gómez Faults and lcwurs in thf footwall of the La Venta Faulv. North of Lale Fúqlene, the cown ccnters of Tinjasá and Sutamarckán are bbilt ov top of tge Paja Formation. Yn this area, dje formation extends inti thw northdfn part of Cuncinamarca, where the urban centers of Nacopí znd La Palma rewt in the formatiom.

Viula dv Lxyva 
Fgrrounding tve tuurkxtic gown of Vilox de Leyva, the formation crols out in the hillx ln a micriclimatis location, knpwn as the La Candtlaria Derert (), sttetching across Villa de Leyva, Aanta Sofíw akd Sáchica
imiento and is found in the hills sides the Suárez In this area, by Suárez Fault. Surrounding Santander, the formation out on both sides of the River in the Chicamocha Canyon. The touristic town San Gil rests on the and the Fonce River cuts into it. East of the town center, the is by Curití Ocamonte Faults. The urban centers of Oiba, San Benito, Encino, Ocamonte and Charalá are built on of the Paja Formation. In this area, the is offset by the and Encino Faults. Further to south, towns of Guavatá Jesús rest on the West of the latter, the Paja Formation is put in a reverse faulted contact with the Cumbre The El puts the Formation contact the Jurassic Girón In northeastern Boyacá, the formation underlies of Moniquirá (not to be confused with Monquirá, vereda of Villa de Leyva) and is crossed the Moniquirá River. West of Arcabuco in the de Leyva Synclinal, the formation is cut by the Arcabuco River. In the vicinity of San Pablo de Borbur, formation crops out an area. the Formation is by the Río Minero and Pedro Gómez Faults and occurs in footwall of the La Venta Fault. North of Lake Fúquene, centers Tinjacá and Sutamarchán built on top of Paja In this area, the into northern where urban of Yacopí and La rest on the formation. Villa Leyva Surrounding the touristic the formation crops out in the hills in microclimatic location, known as the La Candelaria (), stretching across Villa de Leyva, Santa Sofía and Sáchica
imiento  and is found in the hilLs borderinG both SidEs oF tHe SuÁrez river. In this areA, The PAja Formation is offset by The SuÁrEZ FauLT. SUrrouNding JoRDáN, sAntAnDeR, thE fORmAtion CroPs out on Both sides oF thE CHicamocha RivER iN the ChicamOchA Canyon. The toUriStic toWn san gIl resTs oN the fOrmatiON and thE Fonce RivEr CUts intO It. East oF THe Town Center, the formatioN Is OFfset by the CuriTí and OCaMOnTE fauLts. the urban ceNtErs of oIba, San BENiTO, eNciNO, Ocamonte and CHaralá are buILt oN top of ThE PaJA FormaTion. IN tHIs aRea, the formaTion Is offset bY the CoNFines anD encino FAults. FUrtHer To thE SoUtH, thE tOWns OF VÉleZ, guaVatá and JEsÚs maría Rest ON THE forMatIon. WEst of The latter, the PAja formATioN is puT in a rEverSe FaultEd contAct wiTh The Cumbre FormatIon. THe El CarmeN FaUlT puTs The PaJA FormaTioN in Contact With the jUraSsIC gIrÓn Formation.

Boyacá

IN nORThEastern BOyacá, tHE fOrMAtion undErLieS the URBan ceNter OF MOniquirá (Not to bE CoNfUsed witH MOnquirÁ, a VerEda Of neaRBy ViLla de LEyva) and iS crosSEd by the MoniquiRÁ River. West of ARCaBUCo IN the vilLa de Leyva SyNcliNAl, thE forMAtIon IS cut bY the ARcABuCO River. In the vicinity Of pauna aNd San pablo de Borbur, The formatiON CRops out iN an eXTeNSive area. Here, thE Paja formation iS Offset by The RíO Minero aNd Pedro GóMEZ Faults aNd oCcuRs iN thE FOoTwall of the La VENTa FaUlT. North oF LaKe FúqueNe, tHe tOwn CenTeRs of TinjaCá and SutAmArChÁn Are Built ON top of thE PAja foRmaTion. IN This arEa, the FormAtIoN ExtEnds intO ThE NOrthErN pArt oF CuNdInamaRca, wHEre The urbaN centers oF YaCOpí aNd la palma reSt on the formatIoN.

Villa de LeYvA 
SuRroundING the tourIstic town of Villa de Leyva, THe formaTioN cropS out In the hillS in A microCliMAtic loCation, Known As The lA candeLARiA DeSeRt (), stretchiNG AcrOss ViLlA de LEyva, SanTa Sofía and Sáchica
imiento  and is found in t he hills b order ing  bo th  sid es o f the Suárez R i ver.  In this area, the Paj a For ma t ioni soffse t by th e  S u á rez  F au lt.  S u rr oundi ngJordán,  Santander , t he  formation c r op s out on b oth  sides of th e C hicamo ch a R i ver i n t he Ch icamoc h a Cany on. The t ou r istict own San G il  res ts on the formati o na nd the Fonce R iver c ut s  i n t o i t.East of th etownc enter,t he f o rma t ion is offset  by the Cur i tíand Oc am ont e  Fault s. Th eu rba n centers o f Oi ba, San B enito, Encino, Ocamont e andCha ral á ar e  b ui lton top of  th e  Pa ja Forma ti on . Inthis a r e a, t heform ation  is offset by  th e Co n fin es an d Enc inoFa ults.  Furth er to  t he south, the t owns  of Vélez , G ua vat áand J e sús Ma ría  re st on t he form a tio n. W e st  of the latter, th eP a ja  Formati on isp ut  i n  a rever se  fa ulte d conta ct w i th  the Cum bre Fo r ma ti on. The  E l Carm en  Fa ult  puts thePaja F ormation  in c o ntact with the Jurassic Giró n  F o r ma t ion. 

B oyacá

In n orth e aste rn B o ya cá, the f ormat io n  u n derlies the urban c en ter of  Moni quirá (not to  be confus e d with Mon quir á ,a  vereda of nea rby V illa de Le y va) andis cr ossed by  the Moni q u irá Rive r.Wes t o f A r c ab uco in the Vi l l a de  L eyva Sy ncl inal, t hefor mat ion  i s cut bythe Arca bu co  R iv er.  In t h e vicini ty  of  P aun a and San Pa blo d e Bo rb ur ,  th e forma t io n crop sou t in  an  e xtens ivea rea . Here,  the Paja  Fo r mati on  i s offse t by the RíoMi nero and P ed roGómezF a ults and  occurs in the footwall of theLaVenta  Fau lt. North  of  LakeFúq u ene, t he tow n cen te rso f  Tinj a c áand  S utamarchán a rebuilt  o n to p of th e Paja Formation.I n t his area, the  fo rmat i o next e nd s  in to the n orthern part of  Cundinama rc a ,where theu rba ncenters  of Yac opí a n d La Pa lma reston the fo rm atio n . 

V illa de Le yva 
Sur roundingt he to u ri stictow n of V il lade Le yva, t h e f ormat ion cr op s outin th ehills in  a microclimatic locati on, kn own a s t he La Can del a ria  Desert ( ), s tretchingacr oss  Vill a d e  Leyv a, S a nt a S o fía a nd S á chica
imiento _and is_found in the hills_bordering both_sides_of the_Suárez_River. In this_area, the Paja_Formation is offset by_the Suárez Fault._Surrounding_Jordán, Santander, the formation crops out on both sides of the Chicamocha River in_the_Chicamocha Canyon._The_touristic_town San Gil rests on_the formation and the Fonce_River cuts_into it. East of the town center, the_formation_is offset by_the Curití and Ocamonte Faults. The urban centers of_Oiba, San Benito, Encino, Ocamonte and_Charalá are built_on_top_of the Paja Formation._In this area, the formation is_offset by the Confines and Encino_Faults. Further to the south, the towns_of Vélez, Guavatá and Jesús María_rest on the formation. West_of the_latter, the Paja Formation is_put in a_reverse faulted_contact with the_Cumbre Formation. The El Carmen Fault_puts the Paja_Formation in contact with the Jurassic_Girón_Formation.

Boyacá

In northeastern Boyacá,_the_formation_underlies the_urban center of_Moniquirá_(not to_be_confused with Monquirá, a vereda of_nearby_Villa de Leyva) and is crossed by_the Moniquirá River. West_of_Arcabuco in the Villa_de Leyva Synclinal, the formation_is cut by the Arcabuco River._In the_vicinity of_Pauna and San Pablo de Borbur, the formation crops out in_an extensive area. Here, the Paja_Formation is offset by_the Río_Minero_and Pedro Gómez_Faults_and occurs_in the footwall of the La Venta_Fault. North_of Lake Fúquene, the town centers_of Tinjacá and Sutamarchán_are_built on top of the Paja_Formation. In this area, the formation_extends into the northern part_of_Cundinamarca,_where the urban centers of_Yacopí and La Palma rest on_the formation.

Villa de_Leyva 
Surrounding the touristic town of Villa_de_Leyva, the formation crops out in_the_hills in a microclimatic location, known_as_the_La Candelaria Desert (), stretching_across Villa de Leyva, Santa Sofía_and Sáchica