The geologic potentials of Riau Islands Province and its development design by Emi Sukiyah, Vijaya Isnaniawardhani, Adjat Sudradjat, Fery Erawan

“…The morphology exhibits the remnants of peneplain that submerged at ca 13,000 BP now forming Sunda Shelf with the average depth of 120 meters. …”
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Formation Mechanism for Upland Low-Relief Surface Landscapes in the Three Gorges Region, China by Lingyun Lv, Lunche Wang, Chang’an Li, Hui Li, Xinsheng Wang, Shaoqiang Wang

“…It was concluded that the low-relief surfaces in the Three Gorges area did not share a common uplift history, and neither were they peneplain relicts, but rather that the effect of “area-loss feedback” caused by river capture has promoted the formation of upland low-relief surface landscapes. …”
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The Zonation of Landslide Hazard at Kandangan, Temanggung, Central Java by Suratman Woro Suprojo

“…The result of this research are that structural – denudational mountain unit shows highly landslide hazard with sil/debris slide, planar block slide as dominant processes, while in the structural – denudational hills and colluvial valley bottom and river terraces show moderately landslide hazard with soil/debris slide and soil creep as main processes and then in the peneplain and colluvial slope show low landslide hazard. …”
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Impacto ambiental en el geosistema de las canteras de sillar de Añashuayco – Arequipa by Carlos César Trujillo Vera

“…The quarries of Añashuayco are located northwest of the city of Arequipa on a peneplain formedby ignimbrites and alluvionic deposits.The geomorphology of the area is made by a traversal quebrada coming down from the Chachani volcano until its contact with the Chili river in the Uchumayo district, very closeto the La Caldera batholit. …”
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Flore et communautés végétales des inselbergs du Sud-Est du Togo by Fousseni Folega, Kperkouma Wala, Agbelessessi Yao Woegan, Madjouma Kanda, Marra Dourma, Komlan Batawila, Koffi Akpagana

“…On each inselberg, floristic samples (plots of 100 to 500 m2) were carried out along a transect joigning the peneplain to the summit. Each sample plot is also characterized by ecological descriptors. …”
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The changing landforms of Finland by Matti Tikkanen

“…The ancient fold mountains that occupied the area of Finland have been worn down by weathering and erosion processes to form a fairly even peneplain with a mean height above sea level of 154 metres and a maximum height of 1,328 metres (Halti). …”
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Pattern of Karst Landscape of the Cracow Upland (South Poland) by Stefan Witold Alexandrowicz, Zofia Alexandrowicz

“…Their main components are a peneplain crowned by numerous monadnocks, generated as hard-rocks on Upper Jurassic massive limestones (bioherms, carbonate buildups) surrounded by less resistant platy and bedded limestones of the same age. …”
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The wolf spider genus Artoria in New South Wales and the Australian Capital Territory, Australia (Araneae, Lycosidae, Artoriinae) by Volker W. Framenau, Barbara C. Baehr

“…Consequently, the genus mainly occurs east and west along the Great Dividing Range, although some species can be found into the Riverina, Cobar Peneplain and Darling Riverine Plains IBRA regions to the west.…”
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The karst and palaeokarst of North and North-East Greenland – physical records of cryptic geological intervals by Smith, P, Moseley, G

“…The caves of North and North-East Greenland offer a glimpse of large-scale phreatic drainage systems that developed below an uplifted coastal peneplain during Neogene time. They preserve an important part of the geological history of North and North-East Greenland that is otherwise absent from the physical geological record.…”

The Keivy Domain of the Kola Granulite–Gneiss Area on the Baltic Shield: Most Ancient Median Massif of the Continental Crust by Nickolay Sorokhtin, Nikolay Kozlov, Igor Semiletov, Leopold Lobkovsky, Sergey Nikiforov, Dmitry Alekseev, Roman Ananiev

“…Thus, the processes of peneplain formation within the Keivy massif occurred under the cold weather conditions, high volcanic activity in the peripheral zones, and sedimentary cover saturation with the products of the physical and chemical mineral transformation of tonalite–trondhjemite and greenstone rock assemblages. …”
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Cadomian/Pan-African consolidation of the Iberian Massif assessed by its detrital and inherited zircon populations: is the ~610Ma age peak a persistent Cadomian magmatic inheritanc... by Martim Chichorro, Ana Rita Solà, Telmo Bento dos Santos, João Lains Amaral, Lourenço Crispim

“…In Iberia, the opening of the system to Stenian-Tonian detrital zircons during the Ordovician indicates that, at that time, the Trans-Saharan Belt had already become a vast peneplain, which favoured a large drainage system with a long-distance transport mechanism that fed the passive continental margins. …”
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Geochemistry and geochronology of A-type basement granitoids in the north-central Aravalli Craton: Implications on Paleoproterozoic geodynamics of NW Indian Block by Manoj K. Pandit, Hitesh Kumar, Wei Wang

“…The basement granite gneisses from the north-central Aravalli Craton in NW India were investigated for geochemistry and geochronology. In a peneplain terrain, the granite gneiss outcrops are scanty and samples were collected mainly from two small hills and several ground-level exposures in the Sakhun – Ladera region. …”
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The myth of the journey of the soul and Bronze Age funerary sites of the Sintashta and Petrovka type in the Southern Trans-Urals by N.B. Vinogradov

“…The article presents an attempt to interpret the semantics of one of the brightest examples of the burial rite among the pastoral population with high level of metal production, which left the sites of the Sintashta and Pet-rovka type, localized in the Southern Trans-Urals (Trans-Ural peneplain). They are presently dated to the period between the 21st and 18th c. …”
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Cadomian/Pan-African consolidation of the Iberian Massif assessed by its detrital and inherited zircon populations: is the ~610Ma age peak a persistent Cadomian magmatic inheritanc... by Martim Chichorro, Ana Rita Solá, Telmo M. Bento dos Santos, João Lains Amaral, Lourenço Crispim

“…In Iberia, the opening of the system to Stenian-Tonian detrital zircon during the Ordovician indicates that, at that time, the Trans-Saharan Belt had already become a vast peneplain, which favoured a large drainage system with a long-distance transport mechanism that fed the passive continental margins.…”
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Beyond width and density: stable carbon and oxygen isotopes in cork-rings provide insights of physiological responses to water stress in Quercus suber L by Augusta Costa, Paolo Cherubini, José Graça, Heinrich Spiecker, Inês Barbosa, Cristina Máguas

“…In this study, we address the relation between carbon and oxygen stable isotopes of cork rings and precipitation and temperature, in two distinct locations of southwestern Portugal–the (wetter) Tagus basin peneplain and the (drier) Grândola mountains. We aimed at assessing whether the two climatic factors affect cork-ring isotopic composition under contrasting conditions of water availability, and, therefore, if carbon and oxygen signatures in cork can reflect tree functional (physiological and structural) responses to stressful conditions, which might be aggravated by climate change. …”
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Ground motion emissions due to wind turbines: observations, acoustic coupling, and attenuation relationships by L. Gaßner, J. Ritter

“…The investigated wind farms consist of 3 and 16 WTs, respectively, and are located on the Alb peneplain at 700–800 <span class="inline-formula">m</span> height, approximately 300 <span class="inline-formula">m</span> higher than the two municipalities considered in our study. …”
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THE BAIKAL RIFT: PLIOCENE (MIOCENE) – QUATERNARY EPISODE OR PRODUCT OF EXTENDED DEVELOPMENT SINCE THE LATE CRETACEOUS UNDER VARIOUS TECTONIC FACTORS. A REVIEW by V. D. Mats

“…Milanovsky) rift and develops, as shown by the passive rifting model, at the background of the original peneplain until the time when the Baikal region is impacted by stresses resulting from the Indo‐Eurasian collision; the rift structure is a single‐sided basin that comprises the seismically transparent seismostratigraphic complex (SSC‐1); it is bordered at NW by the zone of listric faults. …”
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Karst paleotopography on top of the Dengying Formation and petroleum geological significance in the Central Sichuan Basin, China by Zikun Zhou, Xingzhi Wang, Xiyan Yang, Wenzhi Wang, Hongfei Zhou, Yueming Yang, Long Wen, Fei Huo, Senqi Pei

“…The reconstructed palaeogeomorphology was divided into five types – slopes, erosional peneplains, monadnocks, domes and depressions – according to their morphology, scope and gradient, allowing inference of the palaeohydrological conditions. …”
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Geomorphological Study of the Talumopatu Geothermal Area Gorontalo Regency Gorontalo Province by Hamim Rivaldi Helamsyah Putra, Arifin Yayu Indriati, Manyoe Intan Noviantari

“…In accordance with the results of the analysis, it can be concluded that the geomorphological condition of the study area is divided into three parts, namely the Alluvial Plain Unit, Peneplains Unit, and Residual Hills Unit.…”
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PALEOGEOGRAPHIC SCENARIO OF THE LATE CRETACEOUS – CENOZOIC FOR THE CENTRAL PART OF THE BAIKAL REGION by Victor D. Mats, Irina M. Yefimova

“…In the course of the regional evolution, peneplains altered into uplifted platoes, alpinetype and goltsy mountain ranges; humid quasitropics and subtropics developed into arid zones with the Mediterraneantype climate and moderate and nival zones which were subjected to recurrent mountainandvalley glaciations. …”
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