The goal of this project is to design and construct a small modular autonomous car with room mapping and obstacle avoidance capabilities. The vehicle would be useful in cases where it is dangerous for a human to complete a task, or where it is more efficient to have an autonomous vehicle to scout ahead. A key design goal for this project was also to create an inexpensive platform for research into the realm of autonomous vehicles. The car uses lidar technology to create real time 2D room map and detect obstacles. It is programmed to explore rooms and move without human input. We designed the car with a powerful on board computer, enabling it to run complicated programs and operate without the need of an outside computer.

The goal of this project is to develop a low cost and user-friendly device for remote actuation of light switches. We envision a product that is simple to install, easy to control via a remote, and able to function with a variety of light switch geometries. This device can minimize the inconvenience as well as the risk of injuries from turning the light on and off in the dark, especially for elderly people. For this target end user, the device must be simple and require no technical knowledge. Because of this, we have designed a mechanical actuator that will be mounted to the outside of a light switch without the need for tools and controlled by a simple button remote to be kept at the bedside.

Tracking and recording data from high velocity objects is a difficult task, especially when the object is hidden from view during portions of its flight path. When tasked with this problem, the process of solving it began with copious amounts of research into existing and developing technologies. From thermal imaging to radar detection, many options were explored.
Through a rigorous process of elimination to determine the most efficient and cost effective option, induction coils were chosen as the speed sensing device needed to track the desired objects. Normally when current is induced in one of these coils, there is an unchanging frequency of that current. However, when a conductive material passes through the center of a coil, the original frequency changes. This change can be monitored, giving valuable information about an object's location when evaluated over a specific time period.
After hours of bench top testing, several conclusions were made about the production and effectiveness of the induction coils. Chiefly, it was found that the smaller the induction coil diameter the more effective, the object passing through the coil has a larger effect if it does not pass through the exact center, and the "sweet spot" for the number of coil turns falls between 15-25 turns.

Senior design SRS submission:

For our presentation we hope to speak on three of our major groups of our senior design team:
Our first piece involves using programmable logic controllers (PLCs) that are used as the electrical interface between the programming and the mechanical system. Through its own ladder logic program, the code enables the PLC user to dictate when certain relays should be opened or closed for the purpose of turning on and off the vacuum supply and power sources. The PLC then collects data from the pressure transducers so that a signal indicating the next step is sent back to the design. After reading the pressure associated with a certain head, the user can then close a solenoid valve by sending a signal to it via the PLC which will stop the flow of air. With the PLC, the user is in control of where the flow is going to and is consequently, able to modify it through the code. Although the PLC is not a power supply, it does have the ability of processing information by receiving and sending out specified actions, set by the user, to different electronic and mechanical components.
The second piece is based of a tool from a company called pave more. The “pave more” design is a design that picks up bricks from the hack to a separate location to pack them. The design uses separate heads that pick-up bricks using foam that creates a seal on the brick. The heads are connected to a vacuum that allows us to pick up the bricks efficiently. The heads are each on their own spring system that allows them to be picked up at different heights. They are also each on a separate solenoid valve that will sense a missing brick and close the valve to still allow the system to pick up the bricks. The vacuum system is connected to a filter to protect it from the dust and dirt that are on the bricks.

Habitat loss due to urbanization is a primary cause of declining bat populations globally. As a result of this, research has been conducted to review swimming pools as an alternative source of water for bats in urban areas. After collecting data, GIS analysis utilizing color infrared imagery was performed to assess the impact that residential swimming pools have on bat populations.

In the state of Texas, groundwater resources are utilized for irrigation, mining, municipal use, manufacturing, livestock and steam electric. Over the past 20 years however, there have been shifts and significant trends in groundwater pumpage that can be attributed to changes in annual precipitation, drought, declining industries, and the status of livestock. A multi-year GIS analysis was conducted to analyze trends in Texas Groundwater and the overall factors that impacted pumpage.

South Africa is unique in that the majority of its wildlife is managed in privately owned game reserves. One major challenge for reserves is maintaining healthy stable populations, particularly large species, such as the big five (white rhinoceros (Ceratotherium simum), African elephant (Loxodonta africana), Cape buffalo (Syncerus caffer), African leopard (Panthera pardus), and lion (Panthera leo)). Nevertheless, there has been very little research on management of these charismatic species in such size restricted reserves. To address this need, we are studying the impacts of megaherbivores on the structure and spatial distribution of vegetation in Amakhala Game Reserve. The reserve was created in 1999 from 7,500 ha of agricultural land. Since the formation of the reserve, succession of vegetation has been encouraged to create a more natural environment. However, the introduction of large herbivores, such as elephants and rhinos, may have altered or slowed down this succession. To explore this hypothesis, we conducted a GIS analysis using Landsat imagery and megaherbivore GPS tacking data. Vegetation type was classified to quantify historic changes, and we performed kernel densities and an emerging hotspot analysis with the tracking data (2011-2018) to determine megaherbivore distribution. We determined that the megaherbivores hindered the natural succession of vegetation by maintaining grasslands and preventing woodland encroachment. These findings will facilitate game reserve management by identifying Amakhala’s limitations for increasing browsing herbivores as well as the potential for the addition of grazing herbivores.

Large numbers of migratory tree bats are killed at wind turbines globally. Recent studies have predicted potential population-level impacts as a result, highlighting the need for strategies alleviating bat-wind turbine collisions. Research has shown bats active in close proximity to turbines, approaching and interacting with tower surfaces as if they provided resources, such as water sources and foraging opportunities. Evidence indicates that the smooth surface of the towers can be misperceived by bats as water, and it can also create an acoustic mirror that can enhance foraging success. We hypothesized that a textured coating would disrupt the smooth tower surfaces. Thus, the focus of our study was to determine if texture application would result in decreased bat activity in proximity to tower surfaces, which in turn would reduce collision risk. From May to September 2017, we used thermal cameras, night vision technology, and ultrasonic acoustic bat detectors to assess bat activity at two pairs of wind turbines in north central Texas. Each pair comprised a texture-treated turbine and a control, and bat proximity and behavior at towers were compared. In this first year of testing, we conducted 76 survey nights, observed 1030 confirmed bats on video, and recorded 1215 acoustic calls from 7 bat species. To fully assess the effectiveness of the texture coating, we will be repeating surveys from June to September 2018.

This project will map 2,000-4,000 rare plant species found in Texas. Most of these species have geocoordinates, with some only down to the county-level. These georeferenced plants will be overlaid on to soil type, precipitation, and land development, topography, and ecosystem type maps. This analysis will explain why these habitats are ideal for the rare plants in Texas. Understanding the habitats of these rare plants is important in preserving endangered botanical species. This could lead to a better understanding of this rare biota.

On average, Americans generate about 11.4 million kilograms of spent coffee grounds per day. That is an equivalent weight of a thousand full-size school buses, every day. Most of this coffee is discard, where it eventually ends up in a landfill. However, if recycled or reused this commonly discarded material has many potential uses including as a pest repellent or garden fertilizer. Another use is as a sorbent to remove water contaminants. This means that coffee grounds have the potential to be used as a key component in carbon-based water filters. Evidence from recent research conducted in our laboratory at Texas Christian University shows that charred coffee grounds can effectively remove lead contamination from water. My research will further this work by identifying 1) the specific properties of charred coffee grounds that allows for the removal of lead from water and 2) the optimal temperature for producing charred coffee grounds for water filtration. With the use of infrared spectroscopy and other materials characterization techniques, I will study the properties of charred coffee grounds produced from regular Folgers coffee and an Ethiopian-blend at 250 ℃, 350 ℃, and 450 ℃.

BTEX compounds (benzene, toluene, ethylbenzene, and xylene), and specifically benzene, have been linked to cancer in humans. This project will allow me to develop a map to quantify risk of cancer based the amount of BTEX compounds that have been determined to be in the air. Air pollutant data was gathered by TCEQ using automated gas chromatographs. I collected this data for different monitoring stations in the DFW area in order to compare the differences with Houston. This data was then used to create a map in ArcGIS in order to visualize higher pollution areas. The contaminant levels will then be used with the recommended health exposure levels in order to create a map of risk corridors. This is useful information as it allows individuals to be aware of their personal exposure to these compounds based on the time spent in an area.

Nitrate contamination of groundwater in the Seymour Aquifer is a well-known issue that has been documented since the 1960's. Concentrations as high as 35 ppm NO3-N have been reported, which is a startling 3.5 times the EPA allowable standard for drinking water. While most water from the Seymour Aquifer is used for agricultural irrigation, a portion is still used for domestic purposes and therefore poses a risk to human health. While this problem may have been recognized, the specific source of this contamination remains unknown. Three potential sources of nitrate within the aquifer are being considered in this study—the geological makeup of the aquifer, the agricultural contribution of nitrate from fertilizers, and the historical land use change of the area above the aquifer. My research will combine various analytical and geospatial technologies in order to 1) assess the evolution of groundwater in the Seymour Aquifer since the 1960's, and 2) to determine the source of the high concentrations of nitrate in domestic wells situated on the aquifer. Readily available groundwater quality data from the Texas Water Development Board will be used in conjunction with geospatial analysis and chemical analysis to identify changes in the aquifer's water quality over time. Nitrogen and Oxygen stable isotopic analysis will be used to determine the source of the contaminant. After a thorough analysis of the site area via the aforementioned methods and technologies, a thorough portrait that depicts the source of nitrate contamination in Texas's Seymour Aquifer ought to be painted.

Bats are critical to their surrounding environment, providing numerous beneficial ecosystem services. For instance, they are natural pest controllers, and in urban environments they can control the mosquitoes that cause West Nile Virus. Nevertheless, loss and degradation of habitat, along with disease, have led to declining bat numbers. Restoring and creating suitable habitat will certainly help encourage bats, but first we need to know what resources bats need to survive, such as water. Many available water resources in urban areas, such as streams, ponds, and drainage ditches are ephemeral and dry up during the hot Texas summers. We believe that bats are able to utilize swimming pools in Texas urban areas, thus we explored this by radio-tracking bats in a local park, Foster Park in Fort Worth. We caught bats in this park using a technique called mist netting. Upon capture, we attached a radio-transmitter which emits a signal that can be picked up by a hand-held receiver. We then followed the bats using the transmitter’s signal and triangulated their position every minute to map their nightly routine. From March to September 2017, we tracked a total of 10 evening bats (Nycticeius humeralis). Using ArcGIS, we mapped the bats flight paths and determined home range sizes. From March to May, and September, we found that bats tracked tended to restrict their movement and remained within or near to the park, however from June to August the bats expanded their home ranges and moving longer distances into local neighborhood. This expansion coincided with drying up of water sources within the park, and included areas with swimming pools. Our finding supports the hypothesis that urban habitats have the potential to maintain healthy bat populations, which in turn can aid bat conservation.

Intermittent power outages at Texas and New Mexico border stations has caused significant delays in customs services and information losses through computer shutdowns. The U.S. General Services Administration approached us to address these power quality problems at the border stations through a review of potential distributed generation sources through microgrids to “combat or support” these frequent power outages. The overall aim aside from solving power outages and brown outs at stations is potentially addressing the implementation of renewable energy sources as a power generation for microgrids and coming closer in compliance with Executive Order 13693, “Planning for Federal Sustainability in the Next Decade”. Our approach includes analyzing background information through analysis of GSA documentation and current studies on implementing microgrids in a variety of locations. Current data suggests proposing wind power, solar power, and battery storage based on size and locations of border stations. However, results are pending data collection and GSA input.

Although multiple localized chemostratigraphic and strength studies have been completed on the organic-rich Barnett Shale in the Fort Worth basin (Montgomery et al., 2005; Pollastro et al., 2007; Jarvie et al., 2007; Rowe et al., 2008; Williams et al., 2016; Taylor, 2017; Alsleben, unpublished), basin-wide correlations have not been completed. Basin-wide correlation of chemostratigraphy and mechanical stratigraphy could enhance the understanding of regional variations in chemical composition and rock competence. Therefore, this study is going to test multiple hypotheses to identify regional trends and correlations within the Barnett Shale, based on variations in the formations chemical makeup and rock strength. The purpose is to start establishing a more comprehensive, basin-wide characterization of the mechanical stratigraphy and chemostratigraphic framework of the Barnett Shale in the Fort Worth Basin. Results will start to establish possible regional variations such as rock strength and help determine what controls those variations. Ultimately, the data compilation may provide a better understanding of the Barnett Shale and start to address the complex interactions between marine sediment flux, terrestrial sediment flux, and geochemistry throughout the basin at the time of deposition.

The geomechanical properties of Eagle Ford cores from the San Marcos Arch were measured by hardness tools to test that calcareous rocks are stiffer than the clay-rich shales. Results were quantified and graphed to reinforce the idea that the Maness shale could be more ductile than the superimposing Eagle Ford Shale.

Lithology and facies of the Lower Williams Fork in the Piceance Basin, Colorado were interpreted using spectral gamma ray logs on Petrel. Models were created using this correlated data to predict the facies in an area with no well data. Different modeling methods will be used, such as object modeling and sequence indication simulation to compare and search for the best fit. Published outcrop measurements were used to constrain subsurface geobody geometry. Models were also used to estimate reservoir rock potential in the Lower Williams Fork.

Silica oxides (SiO2) come in a variety of forms including quartz, opal, silica gel and phytoliths. This study will focus on the binding and debinding energetics of sodium benzoate, sodium butyrate and sodium acetate on these various silica oxides. The direct measurement and analysis of binding and debinding energies should provide valuable data and insights into the dynamics of organic molecules at the oxide-water interface. The study will focus on the systematic collection and analysis of experimental data that can be used to support the development, validation and refinement of computational models of interactions involving natural organic matter at the metal oxide-water interface, while facilitating the further development of experiment-driven understanding of binding-debinding dynamics of organic molecules onto mineral surfaces.

METASOMATIC FEATURES IN EUCRITES. R. L. Funderburg1, R. G. Mayne, N. G. Lunning2, and S. Sin-gletary3, 1Monnig Meteorite Collection, 2950 West Bowie Street, SWR 244, Texas Christian University, Fort Worth, TX 76109. (r.funderburg@tcu.edu), 2Department of Mineral Sciences, Smithsonian Institution, National Museum of Natural History, 10th and Constitution NW, Washington, DC 20560-0119. 3Robeson Community College, 5160 Fayetteville Road, Lumberton, NC 28360.

Introduction: The breakdown of pyroxene to silica and troilite was first identified as an alteration process in eucrites by Duke and Silver [1]; however, metasomatism was not iden-tified as a potential cause of these features until the 1990s [2] and has been increasingly identified in the last 10 years [3, 4, 5, 6, 7]. Many eucrite studies were conducted prior to this time and, while metasomatic features may have been identified, they were not attributed to this process.

Barrat et al. [4] proposed a three-stage alteration process to explain the products of metasomatic alteration found in eu-crites:
(1) Fe-enrichments along cracks in pyroxenes
(2) Fe-rich olivine deposits in cracks and troilite
(3) Al-depletion coincident with Fe-enrichment of pyroxene

While metasomatism within eucrites is now commonly identified within the literature, the mechanism for this altera-tion is not well understood. Possible mechanisms proposed in-volve hydrous fluid alteration [4] or sulfurization from a S-rich vapor [6, 7]. The addition of sulfur is required to produce troilite from the breakdown of pyroxene, which has been ob-served in several eucrites [3, 4, 5, 6, 7]. Zhang et al. [5] sug-gested that the sulfur may have been present in the form of a dry S-O-P vapor, formed by the volatilization of pre-existing S- and P-rich material as a result of impacts. Additional petro-logical studies are needed to test if metasomatism was consist-ently driven by S-O-P vapors or if some metasomatism lacks the P-component expected for impact derived vapor.

Metasomatism has been directly investigated for only a handful of eucrites. This study will investigate metasomatism in both Stannern and Main-Group-Nuevo-Laredo (MGNL) eucrites to investigate the com-position of the altering fluid/vapor and overarching processes that drive metasoma-tism on the eucrite parent body. Our preliminary work is fo-cused on the Stannern-trend eucrites Bouvante and LEW 88010, the main group eucrite Béréba, and the polymict eu-crite NWA 4834.

Methods: The samples from this study are on loan from the following: Béréba (USNM 5745-2, USNM 6003-2; Na-tional Meteorite Collection, Smithsonian Institution), Lewis Hills 88010 (LEW 88010) (LEW 88010,4; Meteorite Working Group), Bouvante and Northwest Africa 4834 (NWA 4834) (M1224.3, M1224.5, and M2049.2; Monnig Meteorite Collection). Petrographic analysis was conducted via optical micros-copy with an Olympus BX51 polarizing light microscope at the Oscar Monnig Meteorite Collection at Texas Christian University. Backscatter electron (BSE) maps and major ele-ment data for pyroxenes in Bouvante, LEW 88010, and NWA 4834 were measured by a JEOL JXA-8530F HyperProbe elec-tron microprobe analyzer (EMPA) at Fayetteville State Uni-versity’s Southeastern North Carolina Regional Microanalyti-cal and Imaging Consortium. Backscatter maps were gener-ated for each thin section and energy dispersive x-ray spec-trometry (EDS) point analyses were performed.

Results and Discussion: Of the four samples selected for this study so far, one is unbrecciated (LEW 88010), two are monomict (Béréba and Bouvante), and one is polymict (NWA 4834). These samples were selected as they were observed to contain possible metasomatic features during our petrographic survey, but have not been included in the current literature re-garding metasomatism. They include members of both the Stannern- and MGNL- trends (S: Bouvante and LEW 88010; MGNL: Béréba). All samples are either falls or were observed to show little to no terrestrial alteration. Mineralogically, they are typical eucrites, being dominated by pyroxene and plagio-clase, with lesser phases including troilite, chromite, ilmenite, Fe-rich olivine, and silica.
Preliminary results suggest that Fe-enrichment of pyrox-ene rims, along with an associated Al-depletion, is occurring due to metasomatism in the three samples examined using EMPA. Fe-rich olivine was observed in NWA 4834. Petrographic analysis identified the breakdown of pyroxene into troilite and silica in all four samples.

Future Work: Quantitative pyroxene and plagioclase data for all four samples will be collected prior to the conference. This will allow for further assessment of the Al-depletion along with Fe-enrichment in pyroxenes. We will also investigate the presence of phosphates in these samples to investigate the P-component that would be present in an impact derived vapor. We will assess if there are any differences in metasomatism between MGNL and Stannern-trend eucrites. A survey of previously identified residual eucrites for metasomatic features will also be conducted, so that all three geochemical groupings are represented, if possible.

The Raton Basin of Colorado and New Mexico is a Laramide foreland basin that has been important to coal geology since its first identification as a coal resource in 1821, and as a major Coal Bed Methane resource in the modern era. Raton Basin contains Cretaceous to Paleogene strata representative of the major transgression and subsequent regression of the Western Interior Seaway. The interaction between the distal and proximal lithosomes of strata within the Raton Basin is not fully understood. The coaly, fine-grained rocks of the lower and upper coal zones of the Upper Cretaceous to Paleogene Raton Formation are indicative of deposition in wet, distal lowlands, whereas the coarser grains of the barren series of the Raton Formation indicate that this unit was deposited in a highland setting proximal to the source. While the basin has been explored and produced for petroleum and coal in the past (specifically the Cretaceous Vermejo Formation and Raton Formation), vertical and lateral interaction, geometries, and potential communication between the coal deposits and surrounding fluvial deposits is not well-understood. This project has served as an investigation into the depositional model of the coal deposits and their surrounding fluvial deposits, specifically by: analyzing outcrops using architecture analysis, performing core descriptions and interpretations, conducting coal palynology, organic petrology, and chemical analysis. It has been proposed that the Upper Cretaceous to Paleogene strata of the Raton Basin were deposited within a Distributive Fluvial System (DFS), and that the coal-rich zone is the down-dip expression of this system. Initial results (vertical and lateral relation of facies in core and outcrop, organic petrology, and palynology) reveal that the extensive and laterally continuous coals formed in a woody low-lying fluvio-lacustrine depositional environment, and humid subtropical climate.

The Raton Basin of Colorado and New Mexico is a Laramide foreland basin that has been important to coal geology since its first identification as a coal resource in 1821, and as a major Coal Bed Methane resource in the modern era. Raton Basin contains Cretaceous to Paleogene strata representative of the major transgression and subsequent regression of the Western Interior Seaway. The interaction between the distal and proximal lithosomes of strata within the Raton Basin is not fully understood. The coaly, fine-grained rocks of the lower and upper coal zones of the Upper Cretaceous to Paleogene Raton Formation are indicative of deposition in wet, distal lowlands, whereas the coarser grains of the barren series of the Raton Formation indicate that this unit was deposited in a highland setting proximal to the source. While the basin has been explored and produced for petroleum and coal in the past (specifically the Cretaceous Vermejo Formation and Raton Formation), vertical and lateral interaction, geometries, and potential communication between the coal deposits and surrounding fluvial deposits is not well-understood. It has been proposed that the Upper Cretaceous to Paleogene strata of the Raton Basin were deposited within a Distributive Fluvial System (DFS), and that the coal-rich zone is the down-dip expression of this system. This hypothesis was tested by integrating results from well log correlations, measured sections, architecture analysis of outcrops from drone photogrammetry, core descriptions, and coal palynology and microscopy. Initial results reveal the presence of three distinct, repeating lithosomes (valley-fill sandstones, mixed terminal splays, and very extensive and laterally continuous coals) that are identifiable and correlatable in well logs, are cyclically represented, and suggest basin-scale swings in depositional environment consistent with shifting components within a basin-wide DFS system, consistent with the DFS hypothesis.

The ~1.2 billion-year-old-Barby Formation is located in SW Namibia and has been argued to represent a continental volcanic arc. Previous studies on these rocks primarily relied on mobile-element data, which can be altered by secondary processes and therefore is unreliable for constraining petrologic processes. In an effort to establish the Barby Formation's petrotectonic history, 20 samples were analyzed using XRF and ICP-MS to determine whole-rock major and trace element concentrations. These data were used to answer two questions: (1) Do the samples represent one unique magma series that came from a single source? (2) If the Barby Formation is indeed a volcanic arc, did it form from normal, flat-slab, or oblique subduction? These questions were answered using a combination of geostatisical analyses (distribution, cluster, and outlier analyses), trace-element tectonic discrimination diagrams, and geospatial analyses (see other poster by Lehman et al.). This study supports previous interpretations that the Barby Formation formed in a continental arc setting, with rock samples displaying steeply dipping, light-rare-earth-element enriched patterns, negative Nb/Ta anomalies, and calc-alkaline andesitic to shoshonitic compositions. Major and trace element data indicate at least two magma series from two distinct mantle sources. These two groups are controlled by enrichment differences and variations in the high-field-strength element ratios. The presence of shoshonitic rocks is consistent with flat-slab or oblique subduction.

The ~1.2 billion-year-old-Barby Formation located in SW Namibia has been argued to represent a continental volcanic arc. Recent research by our group (see other poster by Lehman et al.) has supported these arguments with data exhibiting steeply dipping, light-rare-earth-element enriched patterns, negative Nb/Ta anomalies, and calc-alkaline andesitic to shoshonitic compositions. The shoshonitic rocks are particularly interesting as these compositions often form in unusual arc settings (i.e., flat-slab subduction, oblique subduction, ridge subduction). Pearce et al. (2005) showed that the relative plate depth, and in turn, subduction angle and orientation can be interpreted by mapping diagnostic trace element ratios. The spatial distribution of the geochemical ratios could potentially also differentiate between shoshonitic volcanic rocks formed as a result of unusual plate geometries as opposed to a slab tear. If the map displays a tight cluster of shoshonitic composition rocks, the samples more likely formed above a slab tear, while a dispersed arrangement would be more suggestive of either a flat-slab or oblique subduction origin. ArcGis Pro was used to map and analyze XRF and ICP-MS data from 20 samples of the Barby Formation. The samples are from lava flows or sills and range from calc-alkaline to shoshonitic in composition. Both spatial tools and statistical analysis tools were used in an effort to explore potential geospatial relationships of key trace element ratios and previously established geochemical clusters. These results were then employed to attempt to recreate the subduction conditions that formed this volcanic arc.

The depositional model of the Festningen Member of the Barremian Helvetiafjellet Formation is that fluvial to inner deltaic-plain conditions were established as deltas that built southeastward into the Barents Sea basin from an unknown source northwest of present-day Svalbard. Currently, models of Artic drainage provinces are nascent to non-existent. Here, evidence for a large artic drainage basin into the Cretaceous Barents Sea is suggested by using established scaling relationships and the fulcrum method in the Festningen Sandstone.
Data from several locations in Svalbard: Konusdalen, Revneset, Criocerasaksla, and Hanaskogdalen. The Festningen Member sandstone sections were all initially photographed by drone in order to determine channel body dimensions and architecture in the sandstone as well as to record data for 3D photogrammetric construction of virtual outcrop models. Paleohydraulic estimates based on the fulcrum method use bankfull channel dimensions, specifically the height and width, and the D16, D50, D84, and D90 grainsizes to develop basin-process models and infer past catchment constraints. Festningen Member sandstone sections were logged and found to represent braided fluvial systems with mid-channel bars up to 3 m thick and channel-fills up to 4 m thick. Representative bedload samples were taken from approximately 10 cm above the base of channel scours for analysis and model input. The coarse grainsize and large clasts, frequently 3-4 cm and up to 15 cm in diameter, in the Festningen Member sandstone samples show that this was a large river capable of moving a coarse bedload. Scaling relationships equivalent to 4 m channels and coarse grained D-values is on the order of the modern braided Missouri River, on the South Dakota/Nebraska border.
The Bjarmeland Platform and Fingerdjupet Subbasin in the western Barents Sea have a potential petroleum play in the Lower Cretaceous strata, which are, in part, considered to have been fed by the same Festningen fluvial system that is represented in cliff sections on Svalbard. Seismic profiles show clinoforms that may suggest deltaic facies, but remains unknown due to lack of well data.
Seismic data shows that the Cretaceous Festningen fluvial system was able to deliver enough sediments onto the Bjarmeland Platform area to build clinoforms. The size of the source area sufficient to produce a trunk river on this scale remains unconstrained, but an area of at least 100,000 km2 is necessary to produce the river found in the rock record, if the Fulcrum method is applied. Existing Arctic tectonic reconstructions do not consistently show a land area of sufficient size to accommodate this magnitude of drainage area, but results from this study may provide further input to the discussion on timing and land-mass configuration in the present day arctic during the Early Cretaceous.

The 1.2 Ga volcanic arc rocks in the Barby Formation are well exposed in desert terrain in SW Namibia - this formation records the establishment of a major continental margin arc following earlier accretionary events. Recent field work has shown that large portions of the formation consist of pyroclastic fall deposits erupted from small volcanoes (fissures and scoria or spatter cones) in a region with poor drainage and abundant lakes.

Detailed mapping of a well-exposed section of the Barby Formation provides a cross-sectional view of a succession of pyroclastic fall units intercalated with planar bedded lacustrine sediments. Massively bedded units up to ~80 m thick show abundant bombs up to 60 cm across in a matrix of fluidal to angular lapilli, indicating deposition close to source vents undergoing primarily Strombolian-type eruptions. Hypabyssal dikes and sills are common, often cutting through the massively bedded pyroclastic units.

Also present are pyroclastic deposits that intrude lacustrine sedimentary packages at 12 locations spread out over a horizontal distance of ~600 m and a vertical stratigraphic sequence of ~300 m. These deposits contain similar bombs and lapilli as the pyroclastic fall deposits, but show clear fluidal intrusive relations with adjacent sedimentary units. In most cases, zones of peperite are formed in between the pyroclastic intrusions and the lacustrine sediments, consisting of fluidal bodies of vesicular basaltic andesite mingled with fine-grained sediment with preserved lamination. We infer that jets of intrusive pyroclastic material were blasted laterally into weak, unlithified lake sediments from one or more vent conduits feeding explosive eruptions at the surface; these jets are likely to have been forced out by collapse of the conduit inward. Fluidization of the sediment would have occurred as pore water was converted to steam, which would have facilitated lateral motion of the pyroclastic jets.