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A Geologia No Plano De Manejo Do Parque Estadual De Vila Velha, Pr*

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A Geologia No Plano De Manejo Do Parque Estadual De Vila Velha, Pr* Revista Brasileira de Geociencias Mario Sergio de Melo et al. 34(4):56 1-570, dczembro de 2004 A GEOLOGIA NO PLANO DE MANEJO DO PARQUE ESTADUAL DE VILA VELHA, PR* MARIOSERGIODEMELO, LUIZCARLOS GODOY,PAULA MARIELEMENEGUZZO& DIEGOJURASKIPEREIRA DA SILVA Abstract GEOLOG Y IN THE MANA GEMENT PLANOFTHE VILA VELHA STATE PARK. SOUTHERN BRAZIL As a requirementof the managementplanof the Vila Velha State Park(PEVV), ParanaState,Southern Brazil, studiesincludedgeological andgeomorphological mapping, and photointepretationof geological and relief features in several scales(1:70.000 to I:2.000, with fin al maps I:40.(00). The field works and data analysis emphasised main aspects related to the conservation unit. The PEVV is situated inthe easternedgeof the Parana Basin, in a regionstrongly affec ted byfaults, fracturesand dikes related to Mesozoic activity in the PontaGrossa Arch. The geological units present are the Furnas and Ponta Grossa formations (Devonian), the Itarare Group (Carboniferous-Permian), Serra Geral diabase dikes (Lower Cretaceous)and Quaternary alluvial and coluvial sediments. Singular landforms in the PEVV are escarpments, inselbergs, ruiniform landscapes, towers,pinnacles, grikes,corridors, labyrinths, 'furnas' (sinkholes), humiddepressions, ponds, waterfalls, rapids, 'tafoni', solution pans, 'Iapies', alveolus, anastomosed tunnels,corrosion cones, polygonal fractures and termite perforations. The main results of the geological studies concern the indication of specific interest areas or themes for visitation, protection of special areas, recoveryof degraded areas, utilization of adequate construction material, indicationofhazardoussituations,indicationofspecificequipments,indicationof areasfornewattractivcnesscsdevelopment, indicationofthemes for newscientificresearch, indication of priority areas forthe enlargement of the protected perimeter, indication of activities for environmental interpretation, information for the production of printed material and human resources training. Keywords:Vila VclhaState Park, management plan, Furnas Formation, Vila Vel haSandstone. Resumo Estudos geol6gicos realizados no Parquc Estadual de Vila Velha (PEVV) para subsfdio ao plano de manejo ind ufram fotcintepretacao em diversas escalas,trabal hos de campo e producao de mapas geol6gicose geomorfol6gicos em cscala 1:40.000, enfatizando-se aspectos de interesse paraa unidade de conscrvacso. 0 PEVVsitua-sc na borda oriental da Baciado Parana, emarea fonemente afetada porfalhas, fraturas e diques relacionados aatividade mesoz6ica no Arco de PontaGrossa. As unidadesgeologicas que aparecem no parque sao: formacoes Furnas e Ponta Grossa (Devoniano); Grupo Itarare (Carbonlfero-Permiano): diques de diabasio SerraGeral(Eocretacec);sedimentosaluviaisc coluviaisquaternaries. Peicoesde relcvosingularesdo PEVV,que constitucm sua principal razzo de ser, sao: escarpamentos, morros testemunhos, rclevos miniformes; torres e pinaculos; fcndas, corredores e lahirintos:fumas;dcpressces umidas, secase lagoas;cachoeirase corredeiras;lapas:entalhesde base de paredesrochosas;cancluras oucanalctas: bacias de dissoluczo: alvcolos: nineisanastomosadosc cones de erosao:juntas poligonais; pcrfuracoes produzidas por cupins, Os principals subsfdios da Geologia para 0 plano de manejo do PEVV foram: indicacao de areas ou temas de interesse cspecffico paravisitacao;protecac de areascspeciais; rccuperacaode areasdegradadase prcvencaode novos impactos: utilizacao de rnatertais de consrrucaoadequados; indicacao de posslvcis situacocsde risco; tndtcacao de equipamentos especfflc os: indicacjlode areas para descnvolvimentode novos atrativos; indicacao de temas paranovas pesquisas cientificas; indicacao de eventuais areas de amphacao da unidade de conservacao; tndtcacao de atividadcs de lnterpretacac ambiental; producao de material de inform acao, divulgacaoe treinamento;treinamentode recursos humanos. Palavras-chave: Parque Estadual de Vila Velha, plano de manejo, FormacaoFurnas,Arenito Vila Velha. INTRODUC;ii.O Vila Velha ea denorninacao de um notavel ras tectonicas e atect6nicas, processos internpericos e erosivos agrupamento de releva ruiniforme esculpida em arenitos, de gran­ atuantes, dentre outros. Citada como exemplo de a<;ao de proces­ de apelocenico e valor cientifico para a Geologia e Geomorfologia, sos e6licos, este eurn dos mais consagrados equivocos da Iitera­ bern como para estudos arnbientais, vista que 0 relevo de excecao tura geologica e geomorfol6gica brasileira. abriga ecossisrernas tfpicos dos Ca mpos Gerais do Parana, inclu­ Situada cerca de 80 km a WNW de Curitiba e a 20 km a ESE de indo especies da flora e fauna endemicas da regiao, Ponta Grossa (Fig. 1), Vila Velha ha muito tempo notab ilizou-se As esculturas naturais em arenito tern recebido denorninacoes como irnportante p610 de visitacao turfstica, contabilizando-se diversas sugeridas pelo irnaginario dos visitantes leigos: cidade media de 200.000 visitantesla no ao lange da decada de 1990. A cicl6pica, camelo, esfinge, praa do navio, garrafa, tartaruga e a singularidade das esculturas em arenito levou acriacao do Parque taca,estaa simbolo de Vila.Velha, alem de dezenas de outras, cujas Estadual de Vila Velha (PEVV),com 3.122,II ha, pela Lei Estadual alturas variam de poueos metros a cerca de 20 m, distribuidas n" 1.292, de 12 de outubro de 1953. Alern do relevo ruiniforme em numa area corn cerca de 10 ha. a conjunto principal corn relevo arenitos, a parque criado incluiu ainda outras feicoes notaveis, ruiniforme e urn notavel aflorarnento de arenitos periglaciais, de como as furnas e a Lagoa Dourada. genese discutida, onde as esculturas refletem a interacao de vari­ o PEV V foi 0 primeiro parque estadual do Parana . Se por um os fatores:caracterfsticas litol6gicas da rocha sedimentar, estrutu- lado essa antiguidade co ntribuiu para a preservacao de alguns de UEPG - DEGEO, Av. Carlos Cavalcanti 4748, CEP 84.030·900, Ponta Grossa, PR, Brasil, msmelo @uepg.br '" - Trabalho desenvolvido com apoio da Fundacao Araucarin, CNPq c SEMA -Secretaria de Estado do Meio Ambiente e dos Recursos Hfdricos do Parana Revista Brasileira d,e Geodenciee, Volume 34, 2004 561 A geologia no plano de manejo do Parque Estadual de Vila vetne. PR- seus aspec tos naturais, por outre dificultou a adaptacao 11 legisla­ 1:25.ooo e 1:2.000,que apoiaram levantamentos de campo realiza­ c;aoambiental, relativamente recente, Ate 0 ana 2000 0 PEVV ain­ dos entre abril e junho de 2rtY2 . Para dar suporte ao planejamento da era administrado por tres instituicoes com obje tivos muito dis­ do uso da unidade de conservacao (IBAMA 2002), ale m do tintos (turismo, pesquisa agropecuaria e protecao ambiental), e mapeament o de unidades geolog icas foi realizado tarnbem nan existia plano de manejo que disciplinasse sua utilizacao. mapeamento de feicoes geornorfologicas de destaque e de unida­ A partir de 2000, iniciou-se urn esforco de revitalizacao do des de relevo, com mapas finais em escala 1:40.000 (UEPG 2002). PEVV, visando adequa-lo 11 legislacao atual, e dota-lo de plano de a s rnapeamentos e levantamentos foram orientados para atender manejo e infra-estrutura compativelcom a grande visitacao obser­ as diretrizes gerais dos pianos de manejo. vada. Foi neste contexto de revitalizacao que foram realizados os estudos geol6gicos aqui apresentados . GEOLOGIA REGIONAL 0 PEVV localiza-se proximo 11 borda o Decreto n°4.340de2"}J08f2rtY2,que regulamenla lei anterior oriental da Bacia do Parana, cerea de 10 km a oeste do contato que dispoe sobre 0 SNVC - Sistema Nacional de Vnidades de erosivo das unidad es se dimenta res pal eoz6icas sabre 0 Conservacao, indica caracteristicas gerais do plano de manejo: embasamento proterozoico, que aparece a nordeste da area estu­ cstabclecimento dos limites da VC; compatibi lizacao , integracao e dada. Este embasamento ercpresentado por rochas mctamorficas otirnizacao das atividadcs desenvolvidas; regularnentacao da con­ de grau baixo a medic do Supergropo Acungui (Gropo Itaiacoca e cessao de usa pelas populacoes tradicion ais; uniforrnizacao de Formacao Agua Clara, Meso a Neoproteroz6ico, Campanha & conceitos e metodologias; fixacao de diretrizes para 0 diagnostico Sadowski 1998) e vastos cornplexos granit6ides calco-alcalinos da UC; zoneamento; programas de manejo ; estabelecimento de associados (Cunhaporanga, a noroeste da Faixa Itaiacoca, e Tres fases de implerncntacao e de prazos de avaliacao e revisao;carater C6rregos, a sudeste desta faixa). As unidades da Bacia do Parana participativo no manejo; desenvolvimento de pesquisas necessa­ presentes na area estudada sao as formacoes Furnas e Ponta Grossa rias para 0 manejo da DC e area de amortecimento.Tendo em vista (Devoniano), e a base do Gropo Itarare (Ca rbonifero Superior). estas diretrizes gerais. devem ser orientados os levantamentos, Estas unidades estao incluidas nas duas rnegassequen cias basais inclusive os de natureza geologica e geomorfologica, da Bacia do Parana (Assine 1996, Milani et af. 1998). Os estudos geol6gicos nealizados no PEVV nfio diferiram sig­ nificativamente dos procedi mentos usuais em mapeamentos geo­ Formacao Furnas A Formacao Furnas assentadiscordantemen­ 16gicos: foram ulilizadas fotografias aereas em escalas 1:70.000, te sobre rochas do embasamento cristalino ou da Formacao Iapo, r: F • A,u nu du lalhe y..... AreGde Po nla GIII$$1 rlUba + 2 5'30· ) . 49'3 0' Figura 1 - Mapa geologico regional e localiiacdo do Parque Estadual de Vila velha. 1: embasamento proterozoico; 2: Formaciio Furnas ID); 3: Formaciio POllia Grossa
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