Creek Valley Research Articles

Лишайники восточного склона вулкана Берутарубе, о. Итуруп (Курильские острова, Дальний Восток России)

The paper presents an annotated list of lichens of the eastern slope of Berutarube volcano, one of the most inaccessible and poorly studied active volcanoes on Iturup Island. Samples of lichens were collected in August 2023 from eroded areas in the summit part of the volcano, as well as on the eastern slope along the Andrey Creek, in the upper reaches of which unnamed cold acidic springs discharge. In total, 53 species of lichens were identified from the sampling sites, of which 20 species were new to Iturup Island, 2 species were new to the Kuril Islands, and 1 species was new to the Sakhalin region. In the summit part of the volcano, lichens typical for areas of volcanic activity were identified: Cladonia crispata, Cladonia straminea, Huea confluens, Lecidea plana, Melanelia stygia, Pseudephebe pubescens, Rhizocarpon badioatrum, and Umbilicaria torrefacta. The influence of the solfataric gases of the volcano on the lichen biota of the Andrey Creek valley has not been revealed, which allows us to make the assumption that there is no direct influence of the products of the solfataric activity of Berutarube volcano on the natural environment of its eastern slopes.

CAUSES OF THERMAL SUFFOSION ATTENUATION ON THE BESTYAKH TERRACE OF THE LENA RIVER, CENTRAL YAKUTIA

This paper presents the results of thermal suffosion study in the Ulakhan-Taryn Creek valley, Central Yakutia, where intrapermafrost groundwater is discharged. Interpretation of satellite images and analysis of field data from landscape surveys, electrical resistivity tomography studies and ground temperature observations were used to determine the factors contributing to the attenuation of thermal suffosion in sandy deposits of the IV (Bestyakh) terrace of the Lena River. Successional stages of revegetation in the accumulation zones of sands washed off by subsurface flow were examined. Vegetation succession was found to modify geocryological conditions in the groundwater discharge area, sometimes leading to its complete freezing. Conditions favorable both for permafrost aggradation and degradation may develop, depending on the landscape type. Ground temperature data indicate that the active layer thickness in sands at a thermal suffosion site covered by sparse pine forest is 3.5 m, while the mean annual permafrost temperature at the depth of zero annual amplitude is –0.2°С. In 2014, a subaerial talik began to form at this site, the bottom of which lowered from 3.5 m down to 6.0 m. At a larch site with tussocks, the active layer thickness is within 0.5–0.8 m and the mean annual permafrost temperature is about –2.0°С. An ERT survey provided information on the current permafrost and groundwater conditions, where groundwater discharge has ceased. A scenario is proposed describing the changes in the discharge area caused by permafrost disturbance above an aquifer. Formation of an underground cavity and collapse of the overlying permafrost layer resulting in characteristic depressions and sinkholes at the surface promote ground freezing in the discharge zone. Mechanical blocking the flow paths reduces the flow velocity promoting the restoration of permafrost and cutting off the area of soil removal by thermal suffosion. Further on, this attenuates the thermal suffosion. Its active phase can shift spatially due to thawing the pore ice in the permafrost in contact with the confined aquifer, widening soil voids and forming new flow pathways. Thus, attenuation of thermal suffosion on the Bestyakh Terrace of the Lena River results from the combination of internal (impeded flow) and external (vegetation succession) factors.

Geophysical surveys and satellite imaging for the evaluation of near‐surface terrain dynamic – A case study on Grand Portage, MN, USA

AbstractFlooding, erosion and increases in the water level in Lake Superior have contributed to changes in the stem location and width of the Grand Portage Creek. Those events threaten parts of the Grand Portage National Monument, a historically significant site on the North Shore of Lake Superior, Minnesota. We performed geophysical surveys to investigate these dynamic effects. We studied the near‐surface geological deposits, the mechanisms associated with creek stem dynamics and sediment transport, as well as deposition along the lakeshore in Grand Portage Bay. We deployed ground‐penetrating radar (GPR), sub‐bottom profiler, side scan sonar, Geoprobe coring and Van Veen grab samplers and evaluated time‐lapse satellite images to assess the interaction of the Grand Portage Creek with the Grand Portage Bay. The onshore GPR surveys next to the national monument, the creek and the shoreline showed the presence of a complex deposition with eroded ground surfaces and sediment layers across the creek valley. Results from the offshore geophysical campaigns and the interpretations of satellite images also document a heterogeneous deposition sequence environment with fine‐grained sediment deposits present south and southwest of the creek mouth. In addition, we documented an exposed boulder bed towards the east of the creek mouth that was exposed by the current and wave‐driven erosion process in the Grand Portage Bay. Time‐lapse satellite images and hydraulic current velocity simulations validate these observations and provide insight into how anthropogenic activities and natural events interact and might contribute to the long‐term stability of a site of historical and cultural importance.

Stratigraphy and paleoenvironment of the Upper Jurassic Río Damas formation in the Alto Atuel depocenter (Malargüe fold and thrust belt)

The Río Damas Formation is an Upper Jurassic volcano-sedimentary succession, whose outcrops are largely distributed between 33°S and 35.30°S in Chile and Argentina, as part of the retroarc Neuquén Basin fill. This unit was deposited during an important marine regressive phase of the basin. We studied the Río Damas Formation exposures at the Los Gateados creek valley, in the Alto Atuel depocenter (34°40′S; westernmost Malargüe fold and thrust belt), next to the Argentinean-Chilean border. This area represents a key location where the formation interdigitates with the nonmarine red beds of the time equivalent Tordillo Formation, representing a continentalization episode of the Neuquén Basin. This paper presents a lithofacial characterization of the Río Damas Formation, a new U–Pb igneous crystallization age, and a paleographic reconstruction for this period. The Río Damas Formation in the Alto Atuel depocenter consists of porphyritic basaltic and andesitic lavas, interbedded with fine-grained sandstones, conglomerates, volcanic lithic breccias, and pyroclastic deposits. Based on field and petrographic analyses, we associate the Río Damas Formation with a piedmont environment where sedimentary fluvial and alluvial setting coexisted with volcanic effusive and pyroclastic activity. A regional comparison of the Río Damas and Tordillo Formations along the Argentinian-Chilean border shows that the composition and thickness of these units present important latitudinal and longitudinal variations. The increase in thickness and the volcanic component of the Río Damas Formation towards the west could be associated with the proximity to the Jurassic magmatic arc.

Petrographic evidences of open-system magmatic processes in the felsic rocks of the northern part of the Ditrău Alkaline Massif (Eastern Carpathians, Romania)

Abstract Over the almost 190 years-long research of the Ditrău Alkaline Massif (Eastern Carpathians, Romania), felsic rocks have been regarded as homogeneous, uniform units of the igneous complex. Nevertheless, our detailed textural study revealed that the felsic suite (diorite–alkaline feldspar syenite and nepheline-bearing syenite–granite series) cropping out north of the Jolotca Creek valley is more heterogenous at micro-scale than previously thought. This heterogeneity partly derives from abundant mafic mineral-rich clusters; nevertheless, felsic minerals also exhibit various, remarkable textural features. Outcrop to micro-scale traits of felsic crystal settling, mafic mineral aggregates and flow fabrics along with metamorphic country rock xenoliths suggest that the studied rocks crystallized under dynamic magmatic conditions. Cumulate formation, shear flow, convection currents as well as various open-system magmatic processes (e.g., magma recharge, magma mixing and mingling, crystal or mush transfer and recycling, country rock assimilation) played a significant role in the petrogenesis of the examined felsic suite. Based on field observations as well as on the microtextural relationship of the minerals, two major groups of felsic rocks were distinguished: (1) felsic rocks (lacking or containing sparse mafic minerals) spatially associated with mafic rocks and (2) felsic rocks (with mafic minerals and clots) spatially unassociated with mafic rocks. Rocks of the former group are dominated by plagioclase, accompanied by minor alkaline feldspar, biotite and accessory titanite. Distinct structural and textural features suggest the physical accumulation of the rock-forming phases. Such textural properties can also be observed in some rocks of the second group. Isolated mafic minerals are rather scarce in the latter; nevertheless, different types of aggregates made up of either identical or various mafic phases are more common. Clustered minerals are either intact or show different stages of alteration. A detailed petrographic study of the above-mentioned peculiarities has been implemented in order to define their potential origin(s) and petrogenetic significance.

Multi-Dimensional Remote Sensing Analysis Documents Beaver-Induced Permafrost Degradation, Seward Peninsula, Alaska

Beavers have established themselves as a key component of low arctic ecosystems over the past several decades. Beavers are widely recognized as ecosystem engineers, but their effects on permafrost-dominated landscapes in the Arctic remain unclear. In this study, we document the occurrence, reconstruct the timing, and highlight the effects of beaver activity on a small creek valley confined by ice-rich permafrost on the Seward Peninsula, Alaska using multi-dimensional remote sensing analysis of satellite (Landsat-8, Sentinel-2, Planet CubeSat, and DigitalGlobe Inc./MAXAR) and unmanned aircraft systems (UAS) imagery. Beaver activity along the study reach of Swan Lake Creek appeared between 2006 and 2011 with the construction of three dams. Between 2011 and 2017, beaver dam numbers increased, with the peak occurring in 2017 (n = 9). Between 2017 and 2019, the number of dams decreased (n = 6), while the average length of the dams increased from 20 to 33 m. Between 4 and 20 August 2019, following a nine-day period of record rainfall (>125 mm), the well-established dam system failed, triggering the formation of a beaver-induced permafrost degradation feature. During the decade of beaver occupation between 2011 and 2021, the creek valley widened from 33 to 180 m (~450% increase) and the length of the stream channel network increased from ~0.6 km to more than 1.9 km (220% increase) as a result of beaver engineering and beaver-induced permafrost degradation. Comparing vegetation (NDVI) and snow (NDSI) derived indices from Sentinel-2 time-series data acquired between 2017 and 2021 for the beaver-induced permafrost degradation feature and a nearby unaffected control site, showed that peak growing season NDVI was lowered by 23% and that it extended the length of the snow-cover period by 19 days following the permafrost disturbance. Our analysis of multi-dimensional remote sensing data highlights several unique aspects of beaver engineering impacts on ice-rich permafrost landscapes. Our detailed reconstruction of the beaver-induced permafrost degradation event may also prove useful for identifying degradation of ice-rich permafrost in optical time-series datasets across regional scales. Future field- and remote sensing-based observations of this site, and others like it, will provide valuable information for the NSF-funded Arctic Beaver Observation Network (A-BON) and the third phase of the NASA Arctic-Boreal Vulnerability Experiment (ABoVE) Field Campaign.

The Susquehannocks: New Perspectives on Settlement and Cultural Identity

The Susquehannocks: New Perspectives on Settlement and Cultural Identity

Stable isotopes of oxygen and hydrogen in the tap water in the Jalovecký Creek valley in hydrological years 2018–2020

Stable isotopes of oxygen and hydrogen in the tap water in the Jalovecký Creek valley in hydrological years 2018–2020

Preliminary Map Showing Quaternary Geology of the Franklin 7.5-Minute Quadrangle, Indiana

The Franklin 7.5-minute quadrangle is situated near the maximum limit of Wisconsin Episode glacial deposits insoutheastern Johnson County. Till of Wisconsin Episode age (Trafalgar Formation) dominates the surficial geology of thequadrangle. Areas of Wisconsin Episode outwash (Atherton Formation) are found in the Sugar Creek, Youngs Creek, andHurricane Creek valleys and within former meltwater pathways not occupied by modern streams. Kame deposits (sand andgravel) are found in the northern half of the quadrangle and are part of a larger kame complex present in central JohnsonCounty. Holocene (post-glacial) alluvium is found in the valleys of Sugar, Youngs, Nineveh, Buckhart, and Ray Creeks andtributaries. Unconsolidated sediment thickness generally increases from southwest to northeast across the quadrangle, fromless than 15 ft along the southwestern margin of the quadrangle to over 200 ft thick in the far northeastern corner of thequadrangle. This transition of bedrock topography represents the buried northern end of the Knobstone Escarpment. Twosignificant bedrock paleovalleys exist in the quadrangle, one in the south-central part of the quadrangle which parallels theburied Knobstone Escarpment and one in the northeast corner of the quadrangle which is part of a large bedrock valleyextending north into Marion County. The Quaternary sediments in the western half of the quadrangle are underlain byMississippian Borden Group siliciclastic rocks. In the eastern half of the quadrangle, the Devonian New Albany Shale andMuscatatuck Group carbonate rocks subcrop under thick Quaternary sediment cover. The Wisconsin Episode maximumlimit is located within one mile south of the southern boundary of the quadrangle. Radiocarbon ages from the adjacentTrafalgar 7.5-minute quadrangle indicate the Laurentide Ice Sheet reached its maximum extent just after 23,700 years ago. Asecond glacial limit, marked by the Crawfordsville Moraine in the adjacent Trafalgar 7.5-minute quadrangle,crosses the southern end of the Franklin 7.5-minute quadrangle, albeit diffuse. The Crawfordsville Moraine represents thelimit of a readvance which occurred 21,700 years ago. This preliminary geologic map is an interim geologic map product thatdocuments progress in mapping the Quaternary geology of Johnson County, Indiana. The lithologic classification of theQuaternary units of Indiana was used in assigning map units.

Результати досліджень пізньотрипільського поселення Гордашівка-ІІ на Черкащині

Rescue archaeological excavations at the Trypillia settlement of Hordasivka-II (Zvenigorodka district, Cherkassy region) were started in 1996. This settlement is located at western bank of Hirs’kyy Tikych river, in 2.5 km to the west from the south-eastern edge of the village. It is placed on a part of plateau formed by the creek valley from the north and long cavin from the east. Visual observations indicate elliptic structure composed of a single row of dwellings. Settlement size did not exceed 3 ha. The rectangular-shaped Dwelling 1 excavated in Hordashivka (12.5 x 5.0 m) was oriented from north-west to southeast. It is reconstructed as a house with the lower storey’s floor covered by clay and massive ceiling of the lower storey (= floor of the upper storey). Most of the interior details were found on the floor of the lower storey. These are the fireplace, working space, elevations. Collection of finds is mostly represented by pottery (70% of the assemblage is referred to kitchen pottery and 30% of the assemblage is referred to table pottery). Part of the table pottery is decorated in black monochromic painting. Analysis of ceramics allows dating the settlement to Tripolye CII. Considering the relative and absolute chronology (radiocarbon dates obtained for Sharin III), this site may be dated to c. 3400 – 3200 BC. Materials from Hordashivka are “genetically” linked to post-Kosenovskaya group populations in the Southern Bug and Dnieper interfluve. This is traced by the specifics of the technology of vessels production and their decoration. It is important to admit ceramic influences from Sofievskaya group populations in the Middle Dnieper region. Settlements which are chronologically similar to Hordashivka II in the Southern Bug and Dnieper interfluve are not numerous. Later sites in this area are not known, while Trypillia traditions continued in other regions. Keywords: Hordasivka-II, Late Trypillia (C II), settlements, houses, reconstruction, ceramics, chronology.

Do Senohrab jezdí kde kdo

Beginning in 1850, colonies of recreational villas for the upper and upper-middle classes of Prague entrepreneurs and the intellectual elite began springing up in countryside outside of Prague in a radius of 30 kilometres. They were usually established in an agricultural landscape, in river and creek valleys, surrounded by forested hills. The condition was to have a direct rail commute from Prague. As a rule, the establishment of villa colonies was preceded by the stays of Prague denizens in summer flats run by the local farmers or in the local hotels and guesthouses. The actual establishment of the recreational colony was often a business venture of the locals or of Prague entrepreneurs. The recreational villa colony in Senohraby, located on the Emperor Franz Josef Railway near the confluence of Mnichovka Creek and Sázava River, was established as one of the last colonies around Prague by a group of four local as well as Prague developers and constructors in 1895. In 1918, a turn of events in the developments of elite villa colonies for the upper classes of Prague occurred when the Austro-Hungarian Empire fell, or when the independent Czechoslovak Republic was established, respectively. The forests in the proximity of the confluence of the Mnichovka and the Sázava were first overtaken by “tramps” (from the so-called tramping movement) hailing from the lower classes of Prague, and later by conformist recreation-seekers from the middle and lower classes. Despite of being conformist, many such recreation-seekers stylised their abodes-cabins to evoke the non-conformist manner typical for tramping holidays. During World War II, German occupants took over the resort in Senohraby.

Cosmogenic 10Be exposure dating of Bull Lake and Pinedale moraine sequences in the upper Arkansas River valley, Colorado Rocky Mountains, USA

AbstractMany formerly glaciated valleys in the western United States preserve detailed glacial features that span the penultimate glaciation through the last deglaciation; however, numerical age control is limited in many of these systems. We report 35 new cosmogenic 10Be surface exposure ages of moraine boulders in the Sawatch Range, Colorado. Eight ages suggest Bull Lake moraines in Lake Creek (range: 132–120 ka, n = 4) and Clear Creek (range: 187–133 ka, n = 4) valleys may correlate with Marine Isotope Stage 6. In Lake Creek valley, 22 10Be ages from Pinedale end moraines average 20.6 ± 0.6 ka, and 5 10Be ages from a recessional moraine average 15.6 ± 0.7 ka, indicating that glaciers occupied two extended positions at ~21–20 and ~16 ka. The glacial extent dated to ~16 ka was nearly as great as that of the earlier glacial phase, suggesting that climate conditions in the Colorado Rocky Mountains at this time were similar to those of the last glacial maximum. Combining these moraine ages with seven previously published 10Be ages from cirque and valley-bottom bedrock reveals that the Lake Creek paleoglacier lost 82% of its full glacial length in ~1.5 ka and was completely deglaciated by ~14 ka.

Preliminary Map Showing Quaternary Geology of the Mooresville East 7.5-Minute Quadrangle, Indiana

The Mooresville East 7.5-minute quadrangle is situated near the maximum limit of Wisconsin Episode glacial deposits in northeastern Morgan County. Till and outwash of Wisconsin Episode age and Holocene alluvium are the dominant surficial materials in the quadrangle. Wisconsin Episode eolian sand, loess, and colluvium are also present, with eolian sand and colluvium being adjacent to the West Fork White River valley and loess blanketing Wisconsin Episode till and outwash. Holocene (post-glacial) alluvium is found in the West Fork White River and White Lick Creek valleys and tributaries. Mississippian Borden Group bedrock controls many aspects of the surficial geology of the southeastern sector of the quadrangle. For much of this area, bedrock controls the topography and is less than 20 ft below the ground surface. It is mantled on the summits and shoulders of interfluves mainly by Wisconsin till and minor amounts of sand and gravel (outwash) and eolian sand. The depth to bedrock (Borden Group) is greater along the trend of the modern West Fork White River valley, with depths greater than 100 ft. This bedrock paleovalley is filled with mainly Wisconsin Episode outwash (sand and gravel), and the paleovalley was a major path for meltwater in central Indiana during the Wisconsin Episode, from around 27,000 to 19,000 years ago. The Wisconsin Episode maximum limit lies just outside the quadrangle boundary to the south and east. The Laurentide Ice Sheet reached its maximum limit 24,000 years ago, based on radiocarbon dating of organics within till at the terminal moraine in the adjacent Cope quadrangle. Evidence for a readvance of the ice sheet is found in the Mooresville East quadrangle, which occurred 21,700 years ago; the southern limit of the readvance runs through the central part of the quadrangle, just south of State Highway 144.

Hydrogeologic Characterization and Mining Impact Analysis of a Low-Yield, Fractured Granite

A hydrogeologic characterization and impact analysis was performed for a proposed quarry at the Hitch Rack Ranch located in the Little Turkey Creek watershed southwest of Colorado Springs, Colorado. Continuous multiple channel tubing, nested piezometers, stream flow measurements, and mapping of known seeps were used to define the three-dimensional potentiometric distribution and areas of groundwater recharge and discharge. Water balance considerations, mass balance calculations, and potentiometric response to earth tides and barometric fluctuations confirmed that the granite fracture system in the ridge area of the proposed quarry has an extremely low bulk hydraulic conductivity resulting in minimal groundwater discharge to sustain the baseflow of Little Turkey Creek. The Little Turkey Creek valley forms the major conduit for groundwater flow exiting from the upper part of watershed underlain by granite. This conclusion has significant implications with respect to mine planning to minimize projected impacts to the hydrologic system and preserve this recharge component to downgradient Denver Basin sedimentary deposits.

Use of Detailed Topographic Map Evidence of the Southeast Wyoming Gangplank Area to Compare Two Fundamentally Different Geomorphology Paradigms, USA

Drainage divides along a southern Laramie Range crest area and in the nearby southeast Wyoming Gangplank area (as observed on detailed topographic maps) suggest present-day drainage routes in the Cheyenne Tablelands region originated as headward erosion of south-oriented valleys (now the downstream Lodgepole, Crow, and Lone Tree Creek valleys) from an actively eroding northeast-oriented South Platte River valley captured flood flow in the south half of a large east-oriented anastomosing channel complex while headward erosion of a north-oriented valley (now the downstream Horse Creek valley) from the southeast-oriented North Platte River valley captured the north half of the same large anastomosing channel complex. The Gangplank, which today serves as a low gradient ramp of Tertiary Ogallala Formation sediments leading from the Great Plains to the Laramie Range erosion surface, is located along the Crow Creek-Lone Tree Creek drainage divide and low points along that divide (referred to here as divide crossings) suggest, prior to headward erosion of what is now its south-oriented downstream Lone Tree Creek valley, upstream east-oriented Lone Tree Creek drainage routes were intertwined with east-oriented Crow Creek drainage routes, which today flow much further in an east direction (than east-oriented upstream Lone Tree Creek drainage routes) before also turning in a south direction to reach the South Platte River. The ability of the commonly accepted regional geomorphology paradigm to explain this topographic map evidence is then compared with a fundamentally different and new regional geomorphology paradigm’s ability to explain the same evidence. While both paradigms offer possible explanations the new paradigm, which requires headward erosion of the valleys to have occurred as massive continental ice sheet melt water floods crossed the region, explains much more of the drainage system evidence and also permits much more detailed explanations.

Valley reshaping and damming induce water table rise and soil salinization on the Chinese Loess Plateau

A megaproject, “Gully Land Consolidation” (GLC), was launched on the Chinese Loess Plateau in 2011 to combat land degradation and create new farmlands. However, the newly-claimed farmlands have suffered soil salinization, and the mechanism of salinization has been inadequately addressed. In this study, a creek valley that completed the GLC project in 2014 was selected and a total of 17 new farmlands along the reshaped creek valley were investigated in 2016. Moreover, the hillslope farmlands without conducting the GLC project, the loess parent material that used to fill the stream channel, and the water samples from reservoirs, irrigation wells and spring outlets in the reshaped valley were sampled and chemically analyzed. We found that the new farmlands experienced a significant rise in the water table that played a key role on soil salinization. After GLC, >80% of the sampling sites (14 out of 17) showed a shallow depth (≤3 m) from the soil surface down to the groundwater influence zone. Moreover, the closer the downstream farmlands to the newly-built dams, the shallower the water table, indicating considerable impacts of constructing dams on the water table depth in the near-dam farmlands. At the study site, more than half of the shallow soil samples (20 cm depth) underwent light soil salinization, and the most significant soil salinity occurred in the upper stream farmlands. The interplay between a near-surface water table, a high evaporation rate, landform features, and the alkaline properties of the loessial soil has led to the significant soil salinization in the upper stream of the valley. To mitigate soil salinization and ensure the sustainability of the newly-created farmlands in GLC, drainage trenches in the downstream near-dam farmlands and the drainage canals on both sides of the reshaped valley are suggested, which improve the drainage efficiency and control the water table depth.

Geomorphic History of the Beaver Creek Drainage Basin as Determined from Topographic Map Evidence: Eastern Montana and Western North Dakota, USA

The Beaver Creek drainage basin is located along the North Dakota-Montana border slightly to the south of a recognized continental ice sheet margin and immediately to the east of the deep northeast-oriented Yellowstone River valley with Beaver Creek flowing in a north and northeast direction to join the north-oriented Little Missouri River. The Beaver Creek drainage basin originates on an escarpment-surrounded upland and its erosional history was determined by analyzing detailed topographic maps aided by previously made field observations that showed coarse-grained and distinctive alluvium had been transported in an east direction across the Beaver Creek drainage basin and across what is now the deep Little Missouri River valley to sediments making up southwest North Dakota high points containing both the distinctive alluvium and Oligocene age fossils. Drainage divides surrounding the Beaver Creek drainage basin show numerous divide crossings (or notches) linking northwest-oriented Yellowstone River tributary valleys with east-oriented Beaver Creek tributary valleys and west- or northwest-oriented Beaver Creek tributary valleys with southeast- or east-oriented Little Missouri River tributary valleys and suggest the Beaver Creek valley eroded headward across a large-scale flood formed anastomosing channel complex. Buttes located just to the east of the Beaver Creek-Little Missouri River drainage divide suggest the east-oriented water removed as much as 150 meters, or more, of Beaver Creek drainage basin bedrock, and even greater amounts of bedrock from regions to the south of the Beaver Creek drainage basin. Topographic map evidence and routes traveled by the distinctive alluvium suggest a continental ice sheet blocked a large and high-level northeast-oriented river and diverted at least some of the water along the ice sheet margin with the east-oriented floodwaters being captured in a progressive sequence by headward erosion of the Little Missouri River, Beaver Creek, and Yellowstone River valleys (in that order).

Новый чжурчжэньский могильник в Приморье

Purpose. The Manchus’ ancestors, the Jurchen people who established the Jin Dynasty (1115-1234) and the Eastern Xia State (1215-1233) on the territory of the Far East, constructed many sites dated back to those periods in Primorye. Mostly, the sites are walled town, settlements and religious buildings. Up to the present day, the Jurchen burial grounds have remained a highly disputable issue and require more detailed descriptions and more accurate dating. Such a burial ground was found 2 km southeast from the village of Novitskoye in the Partizansky District of Primorye. In the article, we analyze and date the artifacts discovered. Results. The archaeological site is located on the creek valley that is 600 m wide extending from the east to the west. The burial ground is located in a deep mountain glen closed on three sides. Fifteen platform-based graves were excavated there. We have determined that all the bodies buried there had been cremated. The ash was put into a ceramic or wooden urn and then placed onto a flat stone on the bottom of the burial pit. After that, the urn was covered with another flat stone and some wooden pieces. One of the graves was constructed on a high basement decorated with two rows of stones. A «devitalized» (embowed) sword was put over the quiver with eleven arrowheads and some remains of bone dust found on the southwestern side of the basement. A grave house made of river gravels, stones or roofing tiles was erected over the grave. Then the pieces of wood were burnt, all the graveside decorations were covered up with soil. As a result, the grave turned into a small mound. We compared the funeral rites and the constructive features of the burial ground in Novitskoye to those of the previously excavated sites and discovered certain similarities in the cremation rituals and some differences in details of the burial constructions. Conclusion. The burial ground of Novitskoye gives archaeologists an opportunity to outline a more comprehensive concept of the Jurchen funeral traditions of the XII–XIII centuries and associate them with the Buddhist funeral ceremony. It was done by determining the ceremonial features, researching the burial constructions excavated and analyzing their chronological and social contexts.

Topographic Map Analysis of Laramie Range Bedrock-Walled Canyon Complex and the Goshen Hole Escarpment-Surrounded Basin, Albany and Platte Counties, Southeast Wyoming, USA

The Laramie River after flowing in a north direction through southeast Wyoming’s Laramie Basin abruptly turns in an east direction to flow across the north-to-south oriented Laramie Range in a bedrock-walled canyon and eventually reaches the lower elevation Great Plains and southeast-oriented North Platte River. The North Laramie River, Bluegrass Creek, and North Sybille/Sybille Creek also flow from the Laramie Basin in separate bedrock-walled valleys into the Laramie Range before eventually joining the Laramie River. Bedrock-walled through valleys link the various Laramie Range stream and river crossing valleys and detailed topographic maps were used to determine how this anastomosing bedrock-walled canyon complex and the large escarpment-surrounded Goshen Hole basin (located just to the east of the anastomosing canyon complex) originated. Map evidence shows multiple streams of water must have diverged in the Laramie Basin from the north-oriented Laramie River to enter the Laramie Range before converging in or east of the Laramie Range and also shows how present day through valleys enabled diverging and converging streams of water to cross the Laramie Range. The anastomosing bedrock-walled valley complex studied here extends from north of the North Laramie River valley to south of the North Sybille/Sybille Creek valley. Large volumes of water flowing from the Laramie Basin to the Great Plains are interpreted to have eroded the anastomosing canyon complex and the “downstream” Goshen Hole escarpment-surrounded basin. Headward erosion of the north-oriented Sybille and Chugwater Creek valleys across large sheets of east-oriented water are interpreted to have left the Goshen Hole escarpment-surrounded basin as a large abandoned headcut. A water source was not determined, although a continental ice sheet that deeply eroded and warped the North American continent is considered to be a possible source.

Rare-Earth Elements from Modern Mineral–Organic Associations in the Zone of Sulfide Ore Hypergenesis

The REE composition of modern mineral–organic associations in the sulfide ore hypergenesis zone of the Berezitovoe deposit in the Russian Far East was studied for the first time. It is shown that the mineral–organic associations widely abundant in the valley of Konstantinovskii Creek and represented by bright brown crusts on the surface of deluvial deposits were formed at the expense of the influence of acid highly mineralized mine waters from the Berezitovoe deposit. The mineral–organic associations found in the Creek valley may be considered as a new indicator for evaluation of the geoecological state of modern technogenic landscapes.