Cenozoic uplands

Apr 29, 2019 ... ... uplands (67, 70–72). The classifications from the DFA and Whittaker ... The Mid-Cenozoic rise to ecological dominance of open-habitat grasses ...

The Middle Miocene marked the emergence of the Appalachian uplands as a significant sediment source to the Gulf of Mexico. As a result, the Tennessee River joined the Mississippi in creating the dominant fluvial–deltaic depocenter. At the same time, supply from Western Interior uplands decreased. Two Miocene deposodes and multiple ...The Cenozoic Era literally means the era of “modern life.”. It is also called the age of mammals. Mammals took advantage of the extinction of the dinosaurs. They flourished and soon became the dominant animals on Earth. You can learn more about the evolution of mammals during the Cenozoic at the link below. The Cenozoic began 65 million ...Prehistory Proterozoic-Jurassic (pre-local fossil record geologic history) Location of the Iapetus Ocean 550 million years ago. Geological research has revealed a long and complex geological history for the regional now occupied by Louisiana.Preliminary Analytical Results for a Mud Sample Collected from the LUSI Mud Volcano, Sidoarjo, East Java, IndonesiaLow temperature thermochronological constraints on the Cenozoic evolution of the Lake District and Southern Uplands Massifs (NW England, SW Scotland)Kisatchie National Forest, the only National forest in Louisiana, United States, is located in the forested piney hills and hardwood bottoms of seven central and northern parishes.It is part of the Cenozoic uplands (some of Louisiana's oldest rocks) and has large areas of longleaf pine forests (a forest type that has declined significantly over the last century).

It is part of the Cenozoic uplands (some of Louisiana's oldest rocks) and has large areas of longleaf pine forests (a forest type that has declined significantly over the last century). It is one of the largest pieces of natural landscape in Louisiana, with some 604000 acre of public land, more than half of which is vital longleaf pine and ... Jul 26, 2013 ... We are living today in the Holocene epoch of the Quaternary period of the Cenozoic era. Holocene epoch. All the geological activity you see ...Florida. Alluvium (Pleistocene/Holocene) Alluvium - Undifferentiated Quaternary Sediments - Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units.Changes in vegetation, faunal composition, and climate indicate three distinct phases in the Cenozoic evolution of the Central Asian steppe-desert biome (Fig. 5): (i) warm shrub steppe-desert from the middle Eocene, (ii) temperate desert/forested uplands from the EOT to the mid-late Miocene, and (iii) cold-temperate herb steppe from the mid ...The Appalachian Highlands is one of eight physiographic divisions of the contiguous (conterminous) United States. [1] The land area is linked together with the Appalachian Uplands of Canada to make up the Appalachian Mountains. Therefore, from a geographic standpoint, the term Appalachian Highlands is not a synonym for the term Appalachian ...Montane pollen indicates character of mid Cenozoic uplands across Sunda Shelf. ... Their occurrence can be explained by derivation from nearby uplands and thus provide an additional tool to the ...Download Table | The number of trees of each of the six conifer species observed in the 34 100-m2 plots in 1987 and 2008. from publication: Primary conifer succession on a 1915 mudflow in Lassen ...

Cenozoic landforms and post-orogenic landscape evolution of the Balkanide orogen: Evidence for alternatives to the tectonic denudation narrative in southern …Late Cenozoic cooling and changes in glacial–interglacial cycle tempo are thought to increase global rates of erosion starting ~3 million years ago (Ma). Bedrock rivers set rates and patterns of ...Site M0077 includes ∼130 m of impact melt rock and suevite deposited the first day of the Cenozoic covered by <1 m of micrite-rich carbonate deposited over subsequent weeks to years. We present an interpreted series of events based on analyses of these drill cores. Within minutes of the impact, centrally uplifted basement rock collapsed ...Kisatchie National Forest, the only National forest in Louisiana, United States, is located in the forested piney hills and hardwood bottoms of seven central and northern parishes. It is part of the Cenozoic uplands and has large areas of longleaf pine forests. It offers a variety of activities, one being access to all-terrain motorized vehicles. This list of the Cenozoic life of Louisiana contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of Louisiana and are between 66 million and 10,000 years of age. A Abderospira †Abderospira leblanci † ...Uplands on the pre-Ogallala erosional surface are overlain by similar eolian sediments. Buried calcic soils consisting mostly of CaCO, nodules and filaments ...

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The Cenozoic era, which began about 65 million years ago and continues into the present, is the third documented era in the history of Earth. The current locations of the continents and their ...Nov 14, 2004 · The Uplands Province of NE Victoria consists of two petrographically and geochemically similar basalt types of two distinct ages (2.3 and 3.6 Ma) that erupted as flows during peak Pliocene ... Cenozoic potassic-adakitic magmatism initiated at ~45 Ma within a ~200-km-wide elliptical area within the northern Qiangtang terrane, after which it swept westward and southward with time across ...PDF | On Jan 1, 2000, J.E. Johnston and others published Stratigraphic charts of Louisiana | Find, read and cite all the research you need on ResearchGate

Near ~51° S, the proximal Cenozoic Magallanes-Austral Basin preserves shelfal facies overlain by near-shore and continental facies. Documented middle Cenozoic transgressions in Patagonia and Tierra del Fuego have been linked to Cenozoic global sea level rise due to climate [51–53] and phases of Andean orogenesis [50, 54, 55].Download scientific diagram | Cenozoic onshore locations of sediment depositional centers in southern Louisiana (modified after Al Dhamen [2014], Galloway et al. [2001, 2011], Combellas-Biggot and ... Changes in vegetation, faunal composition, and climate indicate three distinct phases in the Cenozoic evolution of the Central Asian steppe-desert biome (Fig. 5): (i) warm shrub steppe-desert from the middle Eocene, (ii) temperate desert/forested uplands from the EOT to the mid-late Miocene, and (iii) cold-temperate herb steppe from the mid ...Florida. Alluvium (Pleistocene/Holocene) Alluvium - Undifferentiated Quaternary Sediments - Much of Florida's surface is covered by a varying thickness of undifferentiated sediments consisting of siliciclastics, organics and freshwater carbonates. Where these sediments exceed 20 feet (6.1 meters) thick, they were mapped as discrete units.Throughout Mesozoic time and part of Cenozoic time, streams wore the Appalachian Mountains down to an almost level surface, or peneplain. During late Cenozoic time, the region was repeatedly arched upward. Uplift gave speed to rivers. They eroded the land, dividing the peneplain into irregular hills and long ridges. The rivers that led to the ...Drylands in central Asia (approximately 40–50°N, 70–105°E) have a very long and complex evolutionary history during the Cenozoic. Previous modeling studies have mainly considered specific geological period and factors; however, few attempts have been made to quantify the role of different factors on the characteristics of central Asian drylands through …Sep 8, 2006 ... Broad, homogeneous basins, separated by mature uplands of moderate to low relief developed across the southwest-draining regional paleoslope.The Coastal Plain Natural Division includes surface deposits from the Cretaceous period of the Mesozoic era (uplands of southwestern Arkansas), the Tertiary period of the Cenozoic era (uplands of south-central Arkansas), and the Quaternary period of the Cenozoic era (alluvial terraces and bottomlands throughout the natural division).The basin contains ~5-km-thick oil-rich Cambrian-Cenozoic strata (Gerhard et al., 1982). During Late Cretaceous time, the Williston Basin might have been incorporated partly into the backbulge depozone of the Cordilleran foreland system (Figure 1a) as a result of the eastward propagation of the thrust belt (Fuentes et al., 2011).Chinese researchers unravel how Qinghai-Tibet Plateau rose to its height. Time：2022-02-14 10:51:46 Source：Xinhua. BEIJING -- Chinese geologists revealed when and how the Central Tibetan Valley elevated from a low valley into its current soaring height, providing new clues to the formation of the roof of the world. The study published ...Trapa natans is widely cultivated in China for its edible fruits (Chen et al., 2007). Macrofossils of Trapa were reported from 11 localities as summarized by Wójcicki et al. (1999), mainly based ...Prehistory Proterozoic-Jurassic (pre-local fossil record geologic history) Location of the Iapetus Ocean 550 million years ago. Geological research has revealed a long and …

a. Primates first evolved on the ground. b. Primates' most special feature is their adaptive versatility. c. Primates were much less geographically widespread in the past than they are today. d. Primates are most similar to tree dwelling rodents. b. Primates' most special feature is their adaptive versatility.

5.1.1 Fluvial to Coastal Sediments: Erosion and the Origin of the Late Cenozoic Sediments. The Barreiras sediments are part of a large clastic wedge of mainly Late Cenozoic age (Pessoa Neto 2003) that is found onshore (Barreiras s.s.) and offshore (Tibau Formation) along the margin of northeast Brazil.They overlie the weathered basement of the coastal …Central Uplands in North Rhine-Westphalia: Siegtal in the Rhenish Massif. The Central Uplands [1] [2] ( German: die Mittelgebirge [3]) is one of the three major natural regions of Germany. It stretches east to west across the country. To the north lies the North German Plain or Northern Lowland; to the south, the Alps and the Alpine Foreland.Subglacial landscapes, revealed in regions of recent ice-sheet retreat, provide a window into ice-sheet dynamics and interactions with evolving subglacial topography. Here, we document landscape evolution beneath the southern Laurentide Ice Sheet of North America since the end of the Pliocene, 2.6 million years (Ma) ago, by reconstructing the ...Dec 8, 2014 ... ... uplands where fires were most likely to burn. If fire activity showed a widespread increase in the late Neogene, as suggested by the ...distribution of upper Cenozoic fluvial basin-fill sediments in the La Bajada constriction area (pl. 2). Stratigraphic Nomenclature and Correlations Fluvial sand and gravel deposited by the ancestral Rio Grande and piedmont sediments derived from uplands to the northeast and northwest of the La Bajada constriction areThe initially rapid expansion of seed plants into unvegetated or sparsely vegetated uplands is considered to have caused enhanced rock dissolution relative to clay formation on end-Devonian continents. ... by analogy with the Late Cenozoic (Raymo & Ruddiman, 1992), or to LIP emplacement, but evidence for such activity during the Late Devonian ...It is part of the Cenozoic uplands (some of Louisiana's oldest rocks) and has large areas of longleaf pine forests (a forest type that has declined significantly over the last century). It is one of the largest pieces of natural landscape in Louisiana, with some 604000 acre of public land, more than half of which is vital longleaf pine and ...

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The Upper Gangetic Plain is marked by uplands with incised rivers and moderately to well-developed soils with salt efflorescence and calcrete. The Plain between Ghaghra, Rapti, Gandak, Baghmati, and Kosi forms a drainage network which, in turn, generated small inland streams. ... The Cenozoic HFB is longitudinally and tectonically dissected by ...Cenozoic Era, Third of the major eras of Earth history, and the interval of time during which the continents assumed their modern configurations and geographic positions. It was also the time when the Earth’s flora and fauna evolved toward those of the present. Central Uplands in Baden-Württemberg: the Kaiserstuhl Central Uplands in North Rhine-Westphalia: Siegtal in the Rhenish Massif. The Central Uplands (German: die Mittelgebirge) is one of the three major natural regions of Germany.It stretches east to west across the country. To the north lies the North German Plain or Northern Lowland; to the …The previously published investigations divided the Cenozoic strata and unconsolidated deposits within the Mississippi Embayment and the Gulf Coastal Plain into 11 major geologic units, typically mapped at the group level, with several additional units at the formational level, which were aggregated into six hydrogeologic units within the ...In central Amazonia, Mesozoic and Cenozoic fluvial deposits- Alter do Chão, Iranduba and Novo Remanso Formations - host supergene iron oxidesand record …Europe - Cenozoic, Igneous, Provinces: From about 60 to 50 million years ago there were important igneous extrusions and intrusions in northwestern Britain. In Northern Ireland and northwestern Scotland, basaltic lava flows (e.g., in the Giant’s Causeway and the northern part of the isle of Skye) are associated with northwest–southeast-trending basaltic dikes and many plutonic (igneous ... Throughout the Cenozoic, the eastern Mediterranean region has been the subject of dramatic tectonic and volcanic activity linked to the convergence and collision between the Eurasian and Afro-Arabic plates and the intervening microplates (Bozkurt, 2001, Maas et al., 2001, Gürbüz and Gül, 2005).The compressional and extensional processes resulting from these …Cenozoic weathering of fluvial terraces in central Amazonia. The iron-lateritic duricrusts developed at top of the Iranduba and Alter do Chão Formations (IR-D1 and ADC-D1) imply that those fluvial deposits were in an upland position above the local erosion base level during the time of goethite and hematite precipitation.It is part of the Cenozoic uplands (some of Louisiana's oldest rocks) and has large areas of longleaf pine forests (a forest type that has declined significantly over the last century). It is one of the largest pieces of natural landscape in Louisiana, with some 604000 acre of public land, more than half of which is vital longleaf pine and ... It is one of the largest pieces of natural landscape in Louisiana, with some 604,000 acres (2,440 km 2) of public land, more than half of which is vital longleaf pine and flatwoods vegetation. These support many rare plant and animal species. ….

The Coastal Plain Natural Division includes surface deposits from the Cretaceous period of the Mesozoic era (uplands of southwestern Arkansas), the Tertiary period of the Cenozoic era (uplands of south-central Arkansas), and the Quaternary period of the Cenozoic era (alluvial terraces and bottomlands throughout the natural division).It is one of the largest pieces of natural landscape in Louisiana, with some 604,000 acres (2,440 km 2) of public land, more than half of which is vital longleaf pine and flatwoods vegetation. These support many rare plant and animal species.Cenozoic weathering of fluvial terraces in central Amazonia. The iron-lateritic duricrusts developed at top of the Iranduba and Alter do Chão Formations (IR-D1 and ADC-D1) imply that those fluvial deposits were in an upland position above the local erosion base level during the time of goethite and hematite precipitation.5.1.1 Fluvial to Coastal Sediments: Erosion and the Origin of the Late Cenozoic Sediments. The Barreiras sediments are part of a large clastic wedge of mainly Late Cenozoic age (Pessoa Neto 2003) that is found onshore (Barreiras s.s.) and offshore (Tibau Formation) along the margin of northeast Brazil.They overlie the weathered basement of the coastal …Feb 14, 2023 · The story of the geology of Arkansas that is visible at the surface begins about 500 million years ago, during the time geologists refer to as the Paleozoic era, or time of “early life.” Today, most rocks that are northwest of a diagonal line running across the state northeast to southwest date from that time. Germany is located at the centre of the map. Germany is located between the geologically very old ( Precambrian) East European Craton ( Baltica) to the north and north-east (that further north is exposed as the Baltic Shield ), and the geologically young (Cenozoic) Alpine - Carpathian Orogen to the south. The corresponding crustal provinces of ...Subglacial landscapes, revealed in regions of recent ice-sheet retreat, provide a window into ice-sheet dynamics and interactions with evolving subglacial topography. Here, we document landscape evolution beneath the southern Laurentide Ice Sheet of North America since the end of the Pliocene, 2.6 million years (Ma) ago, by reconstructing the ...Geology of the Southern Guadalupe Mountains, Texas. CENOZOIC DEPOSITS AND LAND FORMS. THE RECORD OF CENOZOIC HISTORY. The present section of this report deals with the Cenozoic history of the southern Guadalupe Mountains and their surroundings. Here, a different method must be adopted from that used in interpreting Permian history.Five tectono-climatic eras are differentiated: Paleocene late Laramide era; early to middle Eocene terminal Laramide era; middle Cenozoic (Late Eocene-Early Miocene) dry, volcanogenic era; middle Neogene (Middle-Late Miocene) arid, extensional era; and late Neogene (Plio-Pleistocene) monsoonal, epeirogenic uplift era.New insights are gained here by analysing and comparing two independent chronologies—the first based on the chronostratigraphy of existing Cenozoic sedimentary basins, and the second obtained from rock cooling data inferred from four elevated basement uplands situated along a north–south cross-section extending from the External to the ... Cenozoic uplands, PDF | On Jan 1, 2000, J.E. Johnston and others published Stratigraphic charts of Louisiana | Find, read and cite all the research you need on ResearchGate, Appalachian Highlands physiographic division shown by province. The Appalachian Highlands is one of eight government-defined physiographic divisions of the contiguous (conterminous) United States. The land area is linked together with the Appalachian Uplands of Canada to make up the Appalachian Mountains.Therefore, from a geographic standpoint, the term Appalachian …, New insights are gained here by analysing and comparing two independent chronologies—the first based on the chronostratigraphy of existing Cenozoic sedimentary basins, and the second obtained from rock cooling data inferred from four elevated basement uplands situated along a north–south cross-section extending from the External to the ..., Get ratings and reviews for the top 10 gutter guard companies in Upland, CA. Helping you find the best gutter guard companies for the job. Expert Advice On Improving Your Home All Projects Featured Content Media Find a Pro About Please ente..., Request PDF | Constraints on Early Cenozoic underplating-driven uplift and denudation of western Scotland from low temperature thermochronology | Apatite (U–Th)/He and fission track data from ..., data for the Uplands Province basalts and compare them with the Newer Volcanics Province of western- central Victoria. We comment on the enriched geochemical signatures within these Late Cenozoic provinces, in relation to the two cited models, and their relationships to mid ocean ridge basalts (MORB) and oceanic island basalts (OIB) sources., The Cenozoic ( / ˌsiːnəˈzoʊ.ɪk, ˌsɛn -/ SEE-nə-ZOH-ik, SEN-ə-; [1] [2] lit. 'new life') is Earth's current geological era, representing the last 66 million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants. It is the latest of three geological eras, preceded by the Mesozoic and Paleozoic., The peculiar aridity of the region and fragmentation of a once continuous forest belt in equatorial East Africa is linked to the rise of the Ethiopian and East African plateaus during the Late Cenozoic (Spiegel et al., 2007, Pik et al., 2008, Wichura et al., 2010).The uplifted topography of the East African Rift System (EARS) acts as a barrier to air movements related …, Table of Contents. Europe - Cenozoic, Igneous, Provinces: From about 60 to 50 million years ago there were important igneous extrusions and intrusions in northwestern Britain. In Northern Ireland and northwestern Scotland, basaltic lava flows (e.g., in the Giant’s Causeway and the northern part of the isle of Skye) are associated with ..., The Southern Uplands massif may possibly have formed an emergent landmass throughout this interval, but the presence of a Chalk Group sequence in Northern Ireland (Ulster White Limestone Formation) about 130 m thick, and of chalk clasts in volcanic vents in Arran, suggests that chalk deposition encroached across at least the lower lying parts ... , The plains and uplands are generally mantled by Cenozoic sediments. Below these young sediments in the western uplands, and outcropping in places, are relatively un- weathered Archaean schists, quartzites, phyUites, migmatites, gneisses and gneissic granites of the "Gneissic complex" (Fig. 2)., Nov 14, 2004 · The Uplands Province of NE Victoria consists of two petrographically and geochemically similar basalt types of two distinct ages (2.3 and 3.6 Ma) that erupted as flows during peak Pliocene ... , The Cenozoic leaching of rocks by weathering in humid climates—which forms iron-rich residuals (laterization)—also affected the uplands, from northern Queensland to Tasmania. Lastly, during the Pleistocene, small glaciers developed in the Mount Kosciuszko area of New South Wales and the central plateau of Tasmania. , Mesozoic-Cenozoic (251 million years ago-present) Layers of Paleogene rock in eastern Kazakhstan. ... The Triassic was a period of erosion in the Kazakh Uplands and the Zaysan, Alakol, Balkhash and Tengiz basins are all small and filled with Late Triassic through Jurassic lacustrine deposits., Aug 11, 2014 · Planting the Cenozoic Garden. By Riley Black. Published August 11, 2014. • 6 min read. Sixty six million years ago, a global catastrophe extinguished the non-avian dinosaurs. This is common ... , The Gulf Coast Regional Aquifer-System Analysis includes all major aquifer systems in Cenozoic deposits in the Gulf Coastal Plain in the States of Arkansas, Illinois, Kentucky, Louisiana, Mississippi, Missouri, Tennessee, Texas, and small areas in Alabama and Florida (western panhandle area), an area of about 290,000 square miles., The Coastal Plain Natural Division includes surface deposits from the Cretaceous period of the Mesozoic era (uplands of southwestern Arkansas), the Tertiary period of the Cenozoic era (uplands of south-central Arkansas), and the Quaternary period of the Cenozoic era (alluvial terraces and bottomlands throughout the natural division)., Nov 6, 2013 ... The Cenozoic Era (also Cænozoic, Caenozoic or Cainozoic; meaning "new life", from Greek καινός kainos "new", and ζωή zoe "life") is the ..., ... uplands >4 km has existed in the Tibetan Region throughout the Cenozoic, 2) the plateau, although supporting many endemic species, hosts less diversity than ..., The Gulf Coast Regional Aquifer-System Analysis includes all major aquifer systems in Cenozoic deposits in the Gulf Coastal Plain in the States of Arkansas, Illinois, Kentucky, Louisiana, Mississippi, Missouri, Tennessee, Texas, and small areas in Alabama and Florida (western panhandle area), an area of about 290,000 square miles. The Gulf …, Late Cenozoic cooling and changes in glacial–interglacial cycle tempo are thought to increase global rates of erosion starting ~3 million years ago (Ma). Bedrock rivers set rates and patterns of ..., But in Cenozoic, when northern side of the Alborz uplifted, the southern side was under regressive sea with thick layers of pyroclastic-clastic sediments. ... The east and southeast zone is composed of uplands with varying width and altitude, irregular in trend and physiography, and separated by open or basin-like plains. ..., Cenozoic Era, third of the major eras of Earth’s history, beginning about 66 million years ago and extending to the present. It was the interval of time during which the continents assumed their modern configuration and geographic positions and during which Earth’s flora and fauna evolved toward those of the present., Kisatchie National Forest, the only National forest in Louisiana, United States, is located in the forested piney hills and hardwood bottoms of seven central and northern parishes. It …, Montane Pollen Indicates Character of Mid Cenozoic Uplands . Across Sunda Shelf. Bob Morley, Palynova. Exploring the “Undeformed” Bengal Fan and What Lies Below. Romain Courel, Ophir Energy. REFRESHMENT BREAK LUNCH. Exploration in the Central Burma Depression, Onshore Myanmar. Andy Racey, Andy Racey Geoscience, May 15, 2021 · Plateaus are extensive flat uplands found on every continent, as one of the four major landforms on the Earth, among mountains, plains, and hills. Altogether, plateaus take up one-third of the planet's surface, with the largest, the Tibetan Plateau, spreading through Tibet, China, and India, and covering a total of 2.5 million km 2. , geomorphologic systems: Uplands and Plains, Great Endorheic Basins, and Coastal Zone. Based on the interrelationship among these three geomorphological systems the landscape evolution of the late Cenozoic of Península Valdés could be sum-marized in five main stages: (1) development of fluvial and alluvial systems during, The study of paleofluvial dynamics is crucial to understand the role of rivers as biogeographic boundaries in Amazonia during the Cenozoic. In central Amazonia, Mesozoic and Cenozoic fluvial deposits - Alter do Chão, Iranduba and Novo Remanso Formations - host supergene iron oxides and record changes in the distribution of flooded and non-flooded …, The Cenozoic ( / ˌsiːnəˈzoʊ.ɪk, ˌsɛn -/ SEE-nə-ZOH-ik, SEN-ə-; [1] [2] lit. 'new life') is Earth's current geological era, representing the last 66 million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants. It is the latest of three geological eras, preceded by the Mesozoic and Paleozoic., Placing the post-Flood boundary at the Neogene–Quaternary, near the top of the Cenozoic, better explains the rock and paleontological data (figure 1). 15-17 Our conclusion is that all the onshore and the offshore Cenozoic coal beds were produced by the runoff processes late in the Flood. Vast forests of trees living on the pre-Flood uplands ..., Changes in vegetation, faunal composition, and climate indicate three distinct phases in the Cenozoic evolution of the Central Asian steppe-desert biome : (i) warm shrub steppe-desert from the middle Eocene, (ii) temperate desert/forested uplands from the EOT to the mid-late Miocene, and (iii) cold-temperate herb steppe from the mid-late ... , Zhiyuan He (PhD, MSc, B.Eng) is a structural geologist and thermochronologist. He studies lithospheric and crustal deformation of the orogenic belt by using structural analysis and ..., The oil/gas generating reservoir rocks of western offshore fields are exposed in Kutch Basin within the Cenozoic limestone belt and are an excellent scope for studying reservoir ... e.g., Kuar Bet, NW of PU and Kakindia, Karabir, Gorabir, and Gangta Bets (small uplands), which occur between KU and WU. Fault-bounded domes and/or faulted ...