ABSTRATU
Mapeamentu jeolojia no estudu espesialidade fator jeomorfolojia hanesan estudu espesiais, ne’ebe foku ba jeolojia, jeomorfolojia, hidrolojia meterolojia liu husi elaborasaun referensia sira hodi sai hanesan baze ba rekoilamentu dadus iha limitasaun area peskiza. Fator jeomorfolojia mak sai determinante ba rai halai ne’ebe reprezenta risku signifikativu ba vida subsistensia, propriedade, infra-estrutura no rekursu sira ne’ebe parte husi area estudu. Posto Administrativu Bobonaro espesial iha area peskiza konsiste husi arjila mal konsolidasaun ne’ebe mistura ho material heterojenia no heterometika litoklastu kompostu ho bloku bo’ot sira, iha mos mudansa klimatika iha kontekstu geomorfolojika hodi fo espasu ba prosessu akontesimentu rai halai iha area peskiza. Komprensaun konaba prosesu jeomorfolojika ne’e mekanismu fundamentu no importante atu fo susesu ba atividade humana exemplu atividade explorasaun konaba rekursu minerais no planu ordenamentu teritoriu inklui konseitu sira ne’ebe liga ho atividade umanu nian.
Objetivu husi peskizador oinsa atu kontribui liu husi trasforma informasaun konaba faktores jeomorfolojia ne’ebe kontribui ba risku dezastre naturai ne’ebe akontese no husi estudu ida ne’e bele hasa’e mos koinesimentu peskizador nian konaba interpretasaun dadus iha terenu.
Metodu ba elaborasaun dadus monografia tuir etapa sira mak hanesan; akumula referensia, survey ba area peskiza, halo planu ba implementasaun peskiza, prepara ekipamentu, halo mapeamentu no analiza dadus iha laboratorium tuir kurikulum Departamentu Jeolojia.
Rezultadu dadus husi mapeamentu ida ne’e identifika unidade litolojia tolu; unidade kalkariu masivu hola parte iha formasaun Maubisse, unidade kalsilutitu hola parte iha formasaun Aitutu no material malkonsolidasaun mai husi bobonaro mélange. Tipu estrutura iha tolu mak fraktura, faila normal no faila inversa. Forma modelu morfolojia tolu morfografia, deklividade no morfojenesa. Hidrolojia ho tipu mota temporariu no permanente no iha atividade umanu sira. Husi rezultadu ne’e halo produsaun ba mapa sira mak hanesan; mapa pontu parajen, deklividade, morfografia, morfojenesa, unidade jeomorfolojia, jeolojia, solos, estrutura jeolojia, temperatura, presipitasaun, rede hidrografia, basia hidrografia, utilizasaun rai no vejetasaun. Mapa espesifiku ba rai halai mak fator jeolojia, fator klimatiku, fator jeoklimatiku, fator terenu, suceptiblidade , vunerabilidade no risku. Dadus sira ne’e uza sistema semi-kuantitativa katak prepara liu husi operasaun uza aplikasaun Global Mapper, Steronet no ArcGIS 10.4.1 no tuir formatu Kurikulum Departamentu Geologia.
Liafuan Xave: Jeolojia, Jeomorfolojia, Suceptibilidade, Vunerabilidade, Risku.



















ABSTRACT
Geology field camp and study about geomorphology impact as an specialty study in this mapping, focus on geology, geomorphology, hydrology and meteorology, how to getting all reference to accumulation, go to mapping camp to identify all date in this limitation field. The geomorfology is a driver factor to the frequency of landslides. Bobonaro Part of Administration specially in mapping area which mainly consists of poorly consolidated clays and a mixture of highly heterogeneous and heteromorphic litoclastos which include large blocks, also geomorphic and climate context led to very frequent landslide occurrence that characterizes the landscape in this area. The knowledge about of the geomorphological processes and mechanism is a fundamental importance to ensure the success of several happening landside to infect human activities such as the research of natural resources, urban planning and a concept directly linked with the human’s life and activities.
The goal of this work could contribute and transmit about geomorphological characterization information that quantify the degree of susceptibility and risk to natural hazards, particularly to landslides and also to develop how to interpretation about all date in the field camp.
The elaboration of thesis based on those method are; seconder reference elaboration, site survey, field implementation plan, equipment preparation, mapping and interpretation date, laboratory analyses through Geology Department curriculum.
The result of the mapping was identify unite of rock like; massive calcareous unite from Maubisse formation, calcilutite unite from Aituto formation, material unconsolidated from Bobonaro mélange. Three type of structure like fracture, normal fault and reverse fault. Three type of geomorphology like graphic, slope and genetic, the type of hydrology are the temporary river and permanent river also has human activities.
Through date has doing all the map are; stop point, slope, graphic, genetic, geomorphology unite, geology, solos, geology structure, temperature, raining, hydrographic, water direction, land use and vegetation. Specific of landslide like geology factor, climate factor, geology and climate factor, lending factor, susceptibility, vulnerability and final risk. All that date mid quantitative means that was processing with application global mapper, sternest and ArcGIS 10. 4.1 base on the Geology Department Curriculum.
Keywords: Geology, Geomorphology, Susceptibility, Vulnerability, Risk.