Masiro Kanyonu’nun (Pervari) Flüvyo-Karstik Gelişimi ve Yakın Çevresinin Jeomorfik Özellikleri

Zorer, Halil; Öztürk, Yahya

doi:10.26650/jgeog2021-825470

Cited by 4 publications

(3 citation statements)

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“…The change in vegetative cover along the fault plane is due to the different growth of plants in this area (Sipahioğlu et al, 1986). It is seen that some of the faults in the investigation area control the development of vegetation as well as the topography and geomorphic structure (Öztürk and Zorer, 2019;Zorer and Öztürk, 2021). Especially along a fault extending from the south of Kışlacık Village to northwest and a secondary fault extending in SW-NE direction by cutting this fault from its central part, vegetation shows density and linearity (Figure 6, Photo 1c, 1e, 2g, 2f).…”

Section: Tectonic and Lithological Factors On Vegetationmentioning

confidence: 98%

“…Limestones named as Latdağı and Sayındere formations (Şenel, 2008) are massive and have diaclase system. Karst shapes such as lapia, doline, karst canyon and cave have developed in limestones with petrographic texture suitable for karstification (Zorer and Öztürk, 2021). The flysch layers, on the other hand, consist of alternations of marn, sandstone and claystone, and present a red and gray landscape appearance in the topography.…”

Section: Regional Tectonic and Lithologymentioning

confidence: 99%

“…Although studies on subjects such as tectonism and geomorphology have been carried out in the region (Erentöz, 1949;Altınlı et al, 1963;Türkünal, 1980;Öztürk, 2019;Öztürk and Zorer, 2019;Zorer and Öztürk, 2021), researches on the relationship between vegetation and faulting/lithology have not been done. In addition, there is no study on remote sensing assisted analysis of vegetation distribution based on faulty/lithological structure.…”

Section: Introductionmentioning

confidence: 99%

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Faulting and Lithological Features in Vegetation Distribution: A Remote Sensing Asisted Case Study from SE Turkey

Öztürk

TURGAY²,

Çetin

et al. 2023

International Journal of Environment and Geoinformatics

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In this study, the effect of lithological and tectonic parameters on vegetation density was investigated. In this context, two faults and their immediate surroundings in an area whose bedrock is flysch and limestone in the southeast of Turkey (south of Lake Van) were chosen as the sampling area. In the research area, generally, the extensional tectonic regime in NE-SW direction has developed many normal faults and these faults have gained oblique character in places. The aforementioned faults not only controlled the tectonic-morpho dynamics and geomorphic character of the research area, but also controlled the texture of the vegetative cover. For the target purpose of the study, field studies were carried out and remote sensing techniques were applied. GIS and remote sensing outputs (NDVI, lineament, lithological map) and field findings were compared. As a result, it was determined that there were significant relationships between vegetation density in the sampling area, fault lines and lithological features

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Section: Tectonic and Lithological Factors On Vegetationmentioning

confidence: 98%

Section: Regional Tectonic and Lithologymentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 1 more Smart Citation

Faulting and Lithological Features in Vegetation Distribution: A Remote Sensing Asisted Case Study from SE Turkey

Öztürk

TURGAY²,

Çetin

et al. 2023

International Journal of Environment and Geoinformatics

Self Cite

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Environmental Noise Assessment of Residential Buildings with Ground Floor Commercial Function Specific to the Canyon Effect

Bilmez,

Diri

2024

JASA

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Environmental noise is one of the primary important factors that negatively affect human health and quality of life. The canyon effect occurs in the regions between the long structure groups. Canyon effect can cause different conditions in terms of noise, heat, lighting or ventilation. This difference: It depends on the building-road relationship, traffic density, climatic conditions, building dimensions and geometry. Within the scope of this study: The road-structure height relationship of environmental noise specific to street canyons and the trade-housing relationship within the building were examined. Highway was preferred as the sound source. 12 separate operational models were created, and a total of 168 measurement results were obtained from 4 indoor and 10 outdoor measurement points in each model. The results showed the level of the canyon effect specific to different variables.

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Kestel Dağı (Burdur) Batısında Flüvyokarstik Kökenli Polyelerin Jeomorfolojik Özellikleri, Oluşum ve Gelişimleri

Aslan,

Tuncer

2024

Jeomorfolojik Araştırmalar Dergisi

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Burdur ilinin güneyinde KD-GB uzanımlı Kestel Dağı’nın batısında kalan araştırma sahası, yaklaşık 176 km² alana sahiptir. Sahada yüzeylenen kayaların %64’ü karstlaşmaya uygun kayaçlardan oluşur. Kestel Dağı (Burdur) batısında yer alan kısmi karstik litolojiler üzerinde ve aynı zamanda flüvyokarstik süreçlerin birer eseri olan polyelerin oluşum ve gelişim özellikleri ile bu karstik depresyonların morfometrik analizleri araştırılarak açıklanmaya çalışılmıştır. Bu amaçla öncelikle 1/100.000 ölçekli M24 ve N24 jeoloji paftalarından sahanın jeoloji haritası ve jeolojik kesitleri çıkartılmıştır. 1/25.000 ölçekli M24 c4, d3 ve N24 a2, b1 paftaları Coğrafi Bilgi Sistemeleri programlarıyla sayısallaştırılarak bunlardan lokasyon ve jeomorfoloji haritaları üretilmiştir. Sahanın tam ve kısmi karstik özelliklerdeki birimleri üzerinde gelişmiş en yaygın şekiller polyeler, flüvyokarstik vadiler ve dolinlerdir. Bu karstik yapılardan en dikkat çekici olanı da polyelerdir. Sahada glişen polyeler; Bereket, Üçboğaz, Aksu, Yeşildağ, Sinop, Kapaklı, Aziziye ve Bozlar polyeleridir. Sığ karstın en belirleyici şekilleri olan bu polyeler; Pliyosenin sıyrılma yüzeylerinde, özellikle Pliyo-kuvaterner tektonizmasının ve litolojik özelliklerin kontrolünde gelişmiştir. Üst Kretase-Orta Miyosen sonu arasında bölgeye yerleşen bu naplı birimler üzerinde veya birimlerin kontak zonlarında gelişen polyeler, litolojik sınırlarda veya tektonik hatlarda oluştukları için yapısal ve kenar polye karakterindedirler. Bunlar aynı zamanda Pliyosen vadileri üzerinde oluşmuşlar ve Pleistosen ortalarında dış drenaja açılmışlardır. Bu oluşum ve gelişim özellikleriyle çok dönemli-çok kökenli olan bu polyeler, aynı zamanda flüvyokarstik kökenlidirler. Yapılan morfolojik analizlere göre bu polyeler farklı morfolojiler göstermektedir. Tektonik hatların uzanımı, blok faylanmalar, paleo vadilerin uzanımları, morfolojideki gençleşmelerin ortaya çıkardığı flüvyal etkiler nedeniyle polyeler eliptik, yarı eliptik veya uzamış özellikler sunmaktadır. Hesaplanan indis değerlerine göre ise bu polyeler dairesellikten az veya çok uzaklaşmışlardır.

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Masiro Kanyonu’nun (Pervari) Flüvyo-Karstik Gelişimi ve Yakın Çevresinin Jeomorfik Özellikleri

Cited by 4 publications

References 4 publications

Faulting and Lithological Features in Vegetation Distribution: A Remote Sensing Asisted Case Study from SE Turkey

Faulting and Lithological Features in Vegetation Distribution: A Remote Sensing Asisted Case Study from SE Turkey

Environmental Noise Assessment of Residential Buildings with Ground Floor Commercial Function Specific to the Canyon Effect

Kestel Dağı (Burdur) Batısında Flüvyokarstik Kökenli Polyelerin Jeomorfolojik Özellikleri, Oluşum ve Gelişimleri

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