2018
DOI: 10.20502/rbg.v19i3.1342
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Análise E Mapeamento Geomorfológico Da Área De Influência Da Planície Costeira De Pelotas (Rio Grande Do Sul, Brasil)

Abstract: Resumo:Este artigo teve como objetivo elaborar e analisar o mapa geomorfológico da área de infl uência da Planície Costeira de Pelotas, devido à escassez de informações mais detalhadas da Geografia Física do município. Para tanto, obteve-se amparo em orientações metodológicas de Ab'Sáber (1969), União Geográfi ca Internacional (UGI) (DEMEK et al., 1972), Ross (1992) e Instituto Brasileiro de Geografi a e Estatística (IBGE) (2009). O mapeamento adotou a escala 1:125.000 e possibilitou a identifi cação de fatos … Show more

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Cited by 4 publications
(9 citation statements)
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“…The collected horse flies were identified using the methodology described by Silva (2016) and compared to specimens housed in the Entomological Collection of the Federal University of Tocantins (CEUFT). For the identification of the two species, the following characteristics were used ( Silva, 2016 ): the shape of the basal callus, distribution of palp pilosity, and the coloration of the middle tibiae. The coloration of the middle tibiae is darker in T. triangulum ( Figure 1 12, 1.6).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The collected horse flies were identified using the methodology described by Silva (2016) and compared to specimens housed in the Entomological Collection of the Federal University of Tocantins (CEUFT). For the identification of the two species, the following characteristics were used ( Silva, 2016 ): the shape of the basal callus, distribution of palp pilosity, and the coloration of the middle tibiae. The coloration of the middle tibiae is darker in T. triangulum ( Figure 1 12, 1.6).…”
Section: Methodsmentioning
confidence: 99%
“…Besides the polymorphism and overlap in the distribution of both species, they also share many similarities, leading to frequent misidentifications ( Silva, 2016 ) by researchers who are not specialized in the group. These similarities include body size and general coloring, including the color pattern of the tibia ( Figures 1 12, 1.5-1.6), the shape of the frontal callus ( Figures 1 13, 1.7), the frontal indices (FI) and divergence (ID) ( Figures 1 13, 1.7), and the shape of the antenna and palp ( Figures 1 14, 1.8).…”
Section: Introductionmentioning
confidence: 99%
“…Esse relevo se caracteriza por superfícies planas, de declividades inferiores a 2%, de patamares altimétricos alternados: os terraços são predominantes nas faixas altimétricas de 10 a 20 m, as planícies, dos 2 aos 10 m, e o pontal entre as cotas de 1 e 2 m. Os solos são mal drenados, com formação de gleissolos, espodossolos, neossolos flúvicos, planossolos e organossolos (Cunha;Silveira, 1996). As planícies e o pontal compreendem modelados periodicamente inundados pelas águas de escoamento dos corpos lacustre, lagunar, canais fluviais e ou ascensão freática Rehbein, 2018).…”
Section: áRea De Estudounclassified
“…No contexto da Geografia Física, na área do município se observam formas de relevo associados à unidade morfoestrutural da Bacia Sedimentar de Pelotas (planícies e terraços flúvio-lacustres) e do Escudo Sul-Riograndense (colinas, morrotes e morros graníticos), dispostos em amplitude altimétrica de 397 metros (SILVA e REHBEIN, 2018;REHBEIN e DUTRA, 2019, no prelo Ross (1990Ross ( , 1994Ross ( e 2006 2017Fonte: Organizado pelos autores.…”
Section: Nörnberg Rehbeinunclassified