The chalk layer over it however, has been worn away by weathering and time to leave the complex geology of Lower and Upper Greensand, and Gault Clay. The rocks of the national park are also very important because they are the raw material of the soils and some of the rocks are very important in supplying our water.The larger part of Norfolk's bedrock geology is concealed beneath superficial deposits, the oldest of which is a spread of glacial till dating from the Anglian glaciation. Interspersed with the till are sheets of glacial sands and gravels. The fact that the Chalk scarp in East Anglia is much reduced in height compared to its outcrop in ...The Acid Test on Rocks. LIMESTONE, DOLOSTONE, AND MARBLE. Some rocks contain carbonate minerals, and the acid test can be used to help identify them. Limestone is composed almost entirely of calcite and will produce a vigorous fizz with a drop of hydrochloric acid. Dolostone is a rock composed of almost entirely of dolomite. It will …North Landing, Flamborough Head, Yorkshire, a Late Turonian Paramoudra flint in the lower part of the Burnham Chalk Formation below the Ulceby Marl seam (close-up of Fig. 16b). The heavier, more dense flint has sunk into the underlying chalk indicating that flint formation was happening while the chalk was still relatively soft and unconsolidated.Percolation test procedure for surface water soakaways. Step 1. Bore a hole 150mm in diameter with an auger, to a depth of one metre. Step 2. Fill with water to depth of 300mm. As an aid, mark a stick 300mm from one end, place in the hole and fill up to the mark. It takes approximately 5.5 litres to fill a volume of this size.Jun 30, 2018 · Processes of formation of chalk valleys in southern Britain have attracted discussion ever since Martin (1828) referred to “diluvian and meteoric action” to account for the famous Devil’s Dyke coombe near Brighton nearly two centuries ago. Many geomorphological processes and geological influences have been proposed, often reflecting the ... There are various physical properties of Chalk like Hardness, Grain Size, Fracture, Streak, Porosity, Luster, Strength etc which defines it. The physical properties of Chalk rock are vital in determining its Chalk Texture and Chalk Uses. Hardness and Strength of Chalk. The physical properties of Chalk depend on its formation. Oct 21, 2023 · We have since completed about 100 gross Austin Chalk oil wells in that area, capturing 59 million barrels of oil equivalent of reserve potential net to EOG. Shortly following that discovery, we began evaluating the Austin Chalk formation in the Gulf Coast basin and identified its potential as a dry natural gas play in Webb County. The Chalk is the major aquifer of southern and eastern England. It is a microporous white limestone with low matrix permeability. It is an aquifer due to its well developed …Kent; Great Stour; North Downs;. Chalk; Palaeogene; structure; geological model. Front cover. Seaford Chalk in Denne's Chalk. Pit, Canterbury [TR148 566], in.Type Sedimentary Rock Origin Biochemical Texture Nonclastic; Fine-grained Composition Calcite Color White Miscellaneous Massive, Earthy; Reacts with HCl; Hardness < Glass Depositional Environment Deep Marine Geology and Oceanography; chalk. Chalk. gale. views updated Jun 08 2018. Chalk Background. Chalk used in school classrooms comes in slender sticks approximately .35 of an inch (nine millimeters) in diameter and 3.15 inches (80 millimeters) long. Lessons are often presented to entire classes on chalk-boards (or blackboards, as they were ...Geology of Flamborough. The most striking aspect of Flamborough Head is the white chalk cliffs that surround it. The chalk lies in distinct horizontal layers, formed from the remains of tiny sea creatures millions of years ago. Above the chalk at the top of the cliffs is a layer of till (glacial deposits) left behind by glaciers 18,000 years ...Oct 11, 2023 · Chalk can be classified based on various criteria, such as its chemical composition, texture, color, and historical uses. It is categorized …The Ozan unconformably overlies the Austin Chalk. Descriptions of color and composition vary widely because often the descriptions are either state wide summaries or of particular localities. The Geology of Texas Volume 1, Stratigraphy by Sellards, Adkins, and Plummer describe the Ozan as a dark gray marl.09-Feb-2022 ... Chalk is a naturally occurring fine-grained limestone that is formed as a deposit in waters having depth o... · Chalk is a naturally occurring ...Geology of London The geologic foundation. The landscape of southeastern England is shaped by an undulating bed of thick white chalk, consisting of a pure limestone speckled with flint nodules in the upper beds.Feb 20, 2015 · Figure 5, Exposure of Smoky Hill chalk at Goblin Hollow, Sec. 27, T. 13 S., R. 35 W., Logan County, Kansas. General Geology. The Niobrara Chalk has long been classified as part of the Colorado Group, which in Kansas is subdivided as shown in Figure 6. Processes of formation of chalk valleys in southern Britain have attracted discussion ever since Martin (1828) referred to "diluvian and meteoric action" to account for the famous Devil's Dyke coombe near Brighton nearly two centuries ago. Many geomorphological processes and geological influences have been proposed, often reflecting the ...The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault , a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock …Nov 28, 2022 · Chalk is almost pure calcite CaCO3. Other minerals like quartz and clay may also be present with the rock’s 2-4% weight. Chalk is a highly porous rock with 35-47% porosity. Chalk in different colors Chalk Formation. Chalk is produced from fine-grained marine sediment, known as ooze. Oct 15, 2023 · The black crystal is garnet, the pink-orange-yellow colored strands are muscovite mica, and the brown crystals are biotite mica. The grey and white crystals are quartz and (limited) feldspar. Metamorphism is the transformation of existing rock (the protolith) to rock with a different mineral composition or texture.Rock Identification Tips. First, decide whether your rock is igneous, sedimentary or metamorphic. Igneous rocks such as granite or lava are tough, frozen melts with little texture or layering. Rocks like these contain mostly black, white and/or gray minerals. Sedimentary rocks such as limestone or shale are hardened sediment with …A chalk is a soft, friable variety of limestone consisting of poorly lithified calcareous ooze, produced by the accumulation of planktonic organisms in a pelagic (open sea) environment. Chalk is largely made of shells of single-celled marine organisms, such as foraminifera and coccoliths, but fragments of shells of bivalves and ostracods might ...Abstract: The geology of the Chalk beneath east London and the Thames Gateway is reviewed and key features affecting engineering geology are summarized. In ...Chalk engineering geology – Channel Tunnel Rail Link and North Downs Tunnel. Previous. NEXT ARTICLE. 3-D visualization as an aid to the hydrogeological conceptualization of the central South Downs. Next. PDF/EPUB other formats. Contents. Quarterly Journal of Engineering Geology and Hydrogeology. Volume 36, Number 1Chalk is composed of microscopic shells (mostly foraminifera) and has a soft, porous, fine-grained texture. It is formed from the accumulation of microscopic shells in a shallow-water environment. Chalk is commonly white to buff in color. Oolitic limestone is composed of small spherical grains known as oolites that may have a concentric structure.The geology terms channel defines the many processes and occurrences involved with the Earth.. Check out articles with geology terms here at HowStuffW Advertisement Geology terms helps us to explain the phenomena that occurs above, below an...Jan 4, 2022 · Hagiwara mentioned that induction log tool response is a function of vertical and horizontal resistivities, tool configuration, and operating frequency.According to Zhou (), in LWD resistivity logs associated with horizontal and highly deviated wells “horns” are visible when the wellbore crosses a bed boundary.The size of the horn depends on the …Jun 30, 2018 · Section snippets Chalk morphology (dry valleys): overview (CAW) The three sites described under the heading ‘chalk morphology’, Bratton, Devil’s Dyke and Rake Bottom, would initially have been attractive to early geomorphologists and geologists due to their spectacular appearance in comparison with most other chalk dry valleys. Selma Group; Demopolis Chalk (Cretaceous) at surface, covers 17 % of this area. Light-gray to medium-light-gray compact, brittle chalk overlain by abundantly fossiliferous chalky marl, very clayey chalk, and calcareous clay (Bluffport Marl Member). In south-central Montgomery County the Demopolis is split into two eastward extending tongues by ... Learn about the geology of Travis County, Texas, with this comprehensive guidebook that covers the history, stratigraphy, structure, fossils, and mineral resources of the region. The guidebook also includes detailed descriptions and maps of 17 field trips to explore the local geologic features.A chalk is a soft, friable variety of limestone consisting of poorly lithified calcareous ooze, produced by the accumulation of planktonic organisms in a pelagic (open sea) environment. Chalk is largely made of shells of single-celled marine organisms, such as foraminifera and coccoliths, but fragments of shells of bivalves and ostracods might ... The formation, the youngest Chalk preserved in Devon, is confined to small outcrops, in Pinhay Cliffs [SY 312907] and at Beer Head [SY 227 879], both of which are subsided masses that overlie beds of partially dissolved Lewes Nodular Chalk (Gallois, 2005). Up to 1 m of deeply weathered soft white chalk is visible at the highest point of Pinhay ...Jul 14, 2023 · industries. In areas of the UK with a chalk geology we often extract water from the ground (i.e. groundwater) for domestic water supply. Because chalk rivers depend on groundwater for their flow (> 75% of the water in a chalk river comes from the ground) then using groundwater for domestic supply can reduce the level of water in the river.Austin Chalk Overview. The Austin Chalk is an upper Cretaceous geologic formation in the Gulf Coast region of the United States. It is named after type section outcrops near Austin, Texas. The formation is made up of chalk and marl. The Austin Chalk is producing natural gas and oil. Companies drilling the Austin Chalk are having huge success.Chalk engineering geology – Channel Tunnel Rail Link and North Downs Tunnel. Previous. NEXT ARTICLE. 3-D visualization as an aid to the hydrogeological conceptualization of the central South Downs. Next. PDF/EPUB other formats. Contents. Quarterly Journal of Engineering Geology and Hydrogeology. Volume 36, Number 1In Arkansas, chalk is the major constituent of two extensive Cretaceous formations: the Annona Chalk and the Saratoga Chalk. These sedimentary deposits are ...29-Apr-2013 ... Étretat is a coastal region in northern France, well known for its stunning geological landscape. Particularly the headland you see here.Granite is an Igneous rock composed of quartz, biotite, muscovite, feldspars, and occasionally several others, including hornblende, zircon, augite, and magnetite. Typically, granite is between 70 and 77 % silica, 11 to 13% alumina, 3 to 5 % potassium oxide and a smaller percentage containing soda, lime, and iron.Oct 20, 2023 · Glossary. Bedrock deposits: rocks that are older than Quaternary age and generally lithified, which underlie the superficial deposits. Lithomorphogenetic units: geological units that are defined by their shape and mode of origin. They are generally superficial and unnamed, for example unnamed raised beach deposits, glacial moraines …Counties. The Upper Eagle Ford Formation in this region is a mixture of siliciclastic and carbonate sediments. The proportion of carbonate sediments gradually increases upwards to the Base Austin Chalk Unconformity. The sandstones of Upper Eagle Ford Formation have good hydrocarbon reservoir potential based on their non-shale porosity Oct 15, 2023 · Talc, or talcum, is a clay mineral composed of hydrated magnesium silicate, with the chemical formula Mg 3 Si 4 O 10 (OH) 2.Talc in powdered form, often combined with corn starch, is used as baby powder.This mineral is used as a thickening agent and lubricant.It is an ingredient in ceramics, paints, and roofing material.It is a main ingredient …Download this stock image: closeup of sample of natural mineral from geological collection - rough chalk (white limestone) rock isolated on white background ...UK Government reexamines plans for an A303 Stonehenge road bypass tunnel that was originally awarded as one of the Highways Agency’s first Early Contractor Involvement procurements to a construction JV of Balfour Beatty and Costain in 2002. The plan was shelved in 2007 after surveys revealed a risk of encountering radon …The chalk layer over it however, has been worn away by weathering and time to leave the complex geology of Lower and Upper Greensand, and Gault Clay. The rocks of the national park are also very important because they are the raw material of the soils and some of the rocks are very important in supplying our water.Geology is central to the development of Chalk karst with stream sinks concentrated on the Chalk–Paleogene boundary, dolines and dissolution pipes associated with shallow superficial deposits, and subsurface cave, conduit and fissure development concentrated on particular lithological inception horizons.Chalk Formation. The Chalk Formations of Europe are thick deposits of chalk, a soft porous white limestone, deposited in a marine environment during the upper Cretaceous Period. They appear most prominently in England. The formations are divided into three parts: The Upper Chalk, the Middle Chalk, and the Lower Chalk.Email. [email protected]. Haydon is an industrial micropalaeontologist with over 35 years experience in the hydrocarbon exploration and production industry. He started as a specialist in Cretaceous foraminifera with ongoing interests in the biostratigraphy of Late Cretaceous sequences throughout North West Europe and North …The BGS Geological Timechart is based on geochronology. This is the branch of earth sciences that deals with the concept of geological time and dating the sequence of events throughout the Earth’s history. Intervals of …Marl or the other name Marlstone is a calcium carbonate non-clastic sedimentary rock. It has containt variable of clays and silt. The dominant carbonate mineral in the most of the marls calcite, aragonite, dolomite and siderite. Iı belongs to the family of pelitic rocks (clays <0.02 mm, the fine particles in water sales) and a carbonate is a ...Type Sedimentary Rock Origin Biochemical Texture Nonclastic; Fine-grained Composition Calcite Color White Miscellaneous Massive, Earthy; Reacts with HCl; Hardness < Glass Depositional Environment Deep Marine 20 hours ago · It marks 150 years since the first geoscience course was taught at the University of Minnesota! In 1872, professor Edward H. Twining M.A. taught the first courses in geology and mineralogy. 1872 also marks the establishment of the Minnesota Geological and Natural History Survey by the Minnesota State Government.Feb 20, 2015 · Figure 5, Exposure of Smoky Hill chalk at Goblin Hollow, Sec. 27, T. 13 S., R. 35 W., Logan County, Kansas. General Geology. The Niobrara Chalk has long been classified as part of the Colorado Group, which in Kansas is subdivided as shown in Figure 6. The Selma Group is a geological formation in North America, within the U.S. states of Alabama, Mississippi, and Tennessee. The strata date from the Santonian to the Maastrichtian stages of the Late Cretaceous. The group is composed of, in ascending order, the Mooreville Chalk Formation, Demopolis Chalk Formation, Ripley Formation, and Prairie ...Chalk is formed from lime mud, which accumulates on the sea floor in the right conditions. This is then transformed into rock by geological processes: as more sediment builds up on top, and as the sea floor subsides, the lime mud is subjected to heat and pressure which removes the water and compacts the sediment into rock.Feb 19, 2021 · The colonization of the pelagic realm and the massive chalk formation was, from this perspective, rather controlled by environmental parameters than by the evolution of calcareous nannofossils. High sea surface temperatures, vast areas of flooded shelf regions, a sluggish ocean circulation and a low input of nutrients, documented by the absence ... Geology. Chalk. The Hellfire Caves (also known as the West Wycombe Caves) are a network of man-made chalk and flint caverns which extend 260m underground. They are situated above the village of West Wycombe, at the southern edge of the Chiltern Hills near High Wycombe in Buckinghamshire, Southeast England . They were excavated between …Plate 18– Chalk wall [207] Plate 19 – Chalk Wall construction cut [205] Plate 20– Trench 3 –modern rubbish pit Plate 21 – Trench 3- modern pit [307] 4 Archaeological Evaluation of Land adjoining Sunhillow, Gore Lane, Eastry, ... site lies on Bedrock Geology of White Chalk of the Margate Chalk Member.North Landing, Flamborough Head, Yorkshire, a Late Turonian Paramoudra flint in the lower part of the Burnham Chalk Formation below the Ulceby Marl seam (close-up of Fig. 16b). The heavier, more dense flint has sunk into the underlying chalk indicating that flint formation was happening while the chalk was still relatively soft and unconsolidated.Oct 10, 2023 · An evaporite ( / ɪˈvæpəˌraɪt /) is a water- soluble sedimentary mineral deposit that results from concentration and crystallization by evaporation from an aqueous solution. [1] There are two types of evaporite deposits: marine, which can also be described as ocean deposits, and non-marine, which are found in standing bodies of water such ...Type Sedimentary Rock Origin Biochemical Texture Nonclastic; Fine-grained Composition Calcite Color White Miscellaneous Massive, Earthy; Reacts with HCl; Hardness < Glass Depositional Environment Deep MarineThe geology features three distinctive formations of marine origin – the Carstone Formation (orange) at the cliff base, followed above by the Hunstanton Formation (red) formerly known as the Red Chalk, and the Ferriby Chalk (white) extending to the cliff-top (see figures 1 and 2 below). Nov 29, 2022 · The U.S. Geological Survey divides the Cenezoic Era into the Tertiary Period (with the Paleocene, Eocene, Oligocene, Miocene, and Pliocene Epochs) and the Quaternary Period (with the Pleistocene and Holocene Epochs). 2. In millions of years. See also Geologic Timescale. Here are the facts and trivia that people are buzzing about. It is ...Nov 28, 2022 · Chalk is almost pure calcite CaCO3. Other minerals like quartz and clay may also be present with the rock’s 2-4% weight. Chalk is a highly porous rock with 35-47% porosity. Chalk in different colors Chalk Formation. Chalk is produced from fine-grained marine sediment, known as ooze. 26-Nov-2015 ... Delving into the debate - does geology make a difference when it comes to the UK sparkling wine market? World of Fine Wine talks about soil ...The Cretaceous , derived from the Latin “creta” (chalk), usually abbreviated K for its German translation Kreide (chalk), is a geologic period and system from circa 145 ± 4 to 66 million years (Ma) ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the Cenozoic era.25-Jun-2023 ... Chalk is a soft, white, porous, · Chalk, as seen in Cretaceous deposits of Western Europe, is unusual among sedimentary limestones in the ...However, when we interpret the evidence from a biblical perspective, we see that there is an explanation for the formation of these chalk beds that aligns with the biblical timescale of thousands of years. The main cause of these beds is the catastrophic, worldwide Flood. Formation. White chalk is composed almost entirely of calcium carbonate.Reader in Geological Engineering, PhD Undergraduate Year 1 Coordinator Upper cretaceous carbonates (Chalk); Geological disposal of radioactive waste; Geomechanics; Structural geology; Petroleum reservoir characterisation; Modelling slope instability; Coastal recession related to the impact of climate change and weathering of rock.Neogene landform development in southern Britain has been especially controversial. The concept of a Neogene erosion surface (Mio-Pliocene peneplain) on the Chalk of south-east England formed the basis of Wooldridge and Linton’s (1939, 1955 thesis that post-Cretaceous denudation was essentially of Neogene age.chalk, soft, fine-grained, easily pulverized, white-to-grayish variety of limestone.Chalk is composed of the shells of such minute marine organisms as foraminifera, coccoliths, and rhabdoliths. The purest varieties contain up to 99 percent calcium carbonate in the form of the mineral calcite.The sponge spicules, diatom and radiolarian tests (shells), detrital grains of quartz, and chert ...The colonization of the pelagic realm and the massive chalk formation was, from this perspective, rather controlled by environmental parameters than by the evolution of calcareous nannofossils. High sea surface temperatures, vast areas of flooded shelf regions, a sluggish ocean circulation and a low input of nutrients, documented by the absence ...Geology and hydrology. Chalk is a highly porous and permeable rock, and rain falling onto chalk topography percolates directly into the ground, where the chalk layer acts as an aquifer.The groundwater flows through the chalk bedrock, re-emerging lower down the slope in springs.The chalk acts as a temporary reservoir by regulating the amount of water supplied to the springs.Oct 9, 2023 · Geological Survey of Denmark and Greenland Bulletin 2012 | Book EID: 2-s2.0-84863998786 ... The tight danian ekofisk chalk reservoir formation in the south arne field, north sea: Mineralogy and porosity properties. Journal of Petroleum Geology 2012 | Journal article DOI: 10.1111/j.1747-5457.2012.00531.x EID: 2-s2.0-84862673337 ...Oct 11, 2023 · Chalk is a soft, white, porous, sedimentary rock composed primarily of the mineral calcite (calcium carbonate). It is often associated with marine environments and is characterized by its distinctive white color and powdery texture. A Synopsis of Kent's Geology. The rocks that we find at the surface are of Cretaceous and Tertiary age (from about 140 to 50 million years ago). They are a thick sequence of sands, clays and limestones gently folded into an upfold (anticline) known as the Weald Dome. Erosion has removed the highest parts of the dome so that we see the oldest ...Oct 15, 2023 · The black crystal is garnet, the pink-orange-yellow colored strands are muscovite mica, and the brown crystals are biotite mica. The grey and white crystals are quartz and (limited) feldspar. Metamorphism is the transformation of existing rock (the protolith) to rock with a different mineral composition or texture.Chert is a sedimentary rock composed of microcrystalline or cryptocrystalline quartz, the mineral form of silicon dioxide (SiO 2 ). It occurs as nodules, concretionary masses, and as layered deposits. Chert breaks with a conchoidal fracture, often producing very sharp edges. Early people took advantage of how chert breaks and used it to fashion ...
Chalk is a variety of limestone composed mainly of calcium carbonate derived from the shells of tiny marine animals known as foraminifera and from the calcareous remains of marine algae known as coccoliths. Chalk is usually white or light gray in color. It is extremely porous, permeable, soft and friable. Benthic Foraminifera: Scanning electron .... Craigslist new york cars and trucks by owner
floor that geologists believe chalk beds originally formed. The “Problems” for Flood Geology This is the point where critics, and not only those in the evolutionist camp, have said that it is just not possible to explain the formation of the chalk beds in the White Cliffs of Dover via the geological action of the Flood (Flood geology).The Selma Group is a geological formation in North America, within the U.S. states of Alabama, Mississippi, and Tennessee. The strata date from the Santonian to the Maastrichtian stages of the Late Cretaceous. The group is composed of, in ascending order, the Mooreville Chalk Formation, Demopolis Chalk Formation, Ripley Formation, and Prairie ...Geology and Oceanography; chalk. Chalk. gale. views updated Jun 08 2018. Chalk Background. Chalk used in school classrooms comes in slender sticks approximately .35 of an inch (nine millimeters) in diameter and 3.15 inches (80 millimeters) long. Lessons are often presented to entire classes on chalk-boards (or blackboards, as they were ...Chalk Formation. The Chalk Formations of Europe are thick deposits of chalk, a soft porous white limestone, deposited in a marine environment during the upper Cretaceous Period. They appear most prominently in England. The formations are divided into three parts: The Upper Chalk, the Middle Chalk, and the Lower Chalk. Neogene landform development in southern Britain has been especially controversial. The concept of a Neogene erosion surface (Mio-Pliocene peneplain) on the Chalk of south-east England formed the basis of Wooldridge and Linton’s (1939, 1955 thesis that post-Cretaceous denudation was essentially of Neogene age.Jan 24, 2020 · Hearne-area oil. Houston-based Treadstone Energy Partners II LLC is on the northern end of the East Texas Chalk, up on that platform, in the oil window. It has two rigs drilling and plans to average between 1.5 and two rigs at work this year. It’s drilled 20 Chalk wells and five Eagle Ford wells in the area to date. Overview. Kent is the south-easternmost county in England. It is bounded on the north by the River Thames and the North Sea, and on the south by the Straits of Dover and the English Channel. The continent of Europe is a mere 21 miles across the Strait. [2] The major geographical features of the county are determined by a series of ridges ...The Jurassic Coast is a World Heritage Site on the English Channel coast of southern England. It stretches from Exmouth in East Devon to Studland Bay in Dorset, a distance of about 96 miles (154 km), and was inscribed on the World Heritage List in mid-December 2001.. The site spans 185 million years of geological history, coastal erosion having …The Cretaceous , derived from the Latin “creta” (chalk), usually abbreviated K for its German translation Kreide (chalk), is a geologic period and system from circa 145 ± 4 to 66 million years (Ma) ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the Cenozoic era.The formation, the youngest Chalk preserved in Devon, is confined to small outcrops, in Pinhay Cliffs [SY 312907] and at Beer Head [SY 227 879], both of which are subsided masses that overlie beds of partially dissolved Lewes Nodular Chalk (Gallois, 2005). Up to 1 m of deeply weathered soft white chalk is visible at the highest point of Pinhay ...Oct 9, 2012 · As a result, chalk only occurs in parts of east Devon, due to the extensive erosion, but hard flint gravels derived from the chalk are scattered across the county. With a jump in geological time, Devon also contains some younger geological features, namely ball clay deposits and Lundy granite.The lower Anacacho Limestone section of the Taylor Formation followed with an increase in water depth and the introduction of very argillaceous sediments including marly chalk (Ewing, 2013; Loucks ... .
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