The Institute for Geophysics shares data from a range of aerogephysical missions flown over Antarctica.

UTIG has developed, maintained, and operated a suite of aerogeophysical instrumentation since the early 1990s with continual improvements since inception. The suite was installed aboard a Dehavilland DHC-6 ("Twin Otter") up to 2005 and aboard a Basler BT-67 (a version of DC-3T -- a Douglas DC-3 refitted with turboprop engines) since 2008. The current instruments are: High Capability Radar Sounder (HiCARS); Multibeam, Scanning Photon Counting Lidar; Cesium Vapor Magnetometer; Gravimeter; Dual-frequency, carrier-phase Global Navigation Satellite Systems (GNSS); Laser Altimeter; Two GPS-aided Inertial Measurement Units; Three-Axis Fluxgate Magnetometer; System Control, Data Acquisition, and Real-time QC and Monitoring functions.

For fine-scale topographic mapping

Characterizes the chemical properties of water and solids to support research in hydrogeology, geochemistry, and geomicrobiology. Equipment used: carbon analyzer (TC), Organic analysis Field and laboratory gas chromatographs, thermal desorber, high pressure liquid chromatographs, Inorganic analyses Ion chromatograph, autotitrator, field and lab spectrophotometers. BET sorptometer for N2, Ar, and Kr BET surface areas, and A microporosities, organic carbon analyzer.

The Austin Core Research Center (CRC), located adjacent to Bureau headquarters, is the Bureau of Economic Geology's main core repository for core and rock material donated to the university. More than 500,000 boxes of core and cuttings from wells drilled throughout Texas, the U.S., and the world are available at this facility for public viewing and research. Austin, Houston, and Midland core facilities have combined holdings of nearly 2 million boxes of geologic material. The Integrated Core and Log Database (IGOR) is a searchable database for all CRC core and well cutting holdings. Public facilities include core examination layout rooms and processing rooms for slabbing core. Other services are available upon request.

The Houston Research Center (HRC), is located on the west side of Houston, Texas, six miles north of I-10 and two miles south of U.S. Highway 290. This state-of-the-art climate-controlled facility is equipped to permanently store and curate over 900,000 boxes of geologic core and cuttings. The Houston, Austin, and Midland core facilities have combined holdings of nearly 2 million boxes of geologic material. In addition to the climate-controlled core and cuttings warehouse, the HRC complex has offices, laboratories, and a well-lit core layout room available for visiting scientists. There are also two conference rooms to accommodate guests attending short courses and seminars. Other services are available upon request. Nominal fees are charged to rent table space and to view core. The HRC has space dedicated for storing samples and cores acquired by NSF-funded research. The HRC curates this material and facilitates continued access to the material by researchers. The Integrated Core and Log Database (IGOR) is a searchable database for all core and well cutting holdings.

We have 5 Trimble Net-RS receivers, tripods, choke ring antennas. One is with Tiffany Caudle at BEG used to support the Optech Lidar system. The other 4 are in JGB 3.122 and used by various groups.

Installed in 2002-2003, the JEOL JXA-8200 electron probe microanalyzer (EPMA) is equipped with five wavelength dispersive spectrometers (WDS), an energy dispersive detector (EDS), and two image detectors in secondary and backscattered electron modes. The primary aim of the microprobe is quantitative elemental analysis of minerals on a microscale with high precision (less than a percent relative for major constituents) and low detection limits (commonly a few tens to few hundreds ppm)

The Flash Flood and Tsunami flume is a large (approximately 40 x 1.5 x 0.8 m) outdoor flume with a computer-controlled headbox lift gate that generates reproducible flood bores. It is being used to study the hydraulics and sediment transport of rapidly changing hydrographs.

We have a custom built, low-frequency, short-pulse, ground-based radar system to image deep (>100 m) internal layers and the base of the ice sheet. Frequencies used with this system include 1, 2, 5 and 10 MHz. We also have a GSSI high-frequency (100MHz) ground-based radar system which can be used in several configurations and with a range of antennae frequencies. In addition, we have 7 GNSS GPS units for high-precision positioning, as well as multiple data loggers and time-lapse cameras for use in glaciological settings.

This laboratory contains Ro-tap seiving apparatus, a Micromeritics 5100 clay and silt size x-ray analyzer, and an automated settling column for sizing sand fraction.

This lab is dedicated to hydrogeology and environmental geology courses. It has facilities for grain-size analyses, porosity/ permeability testing, and a wide variety of lab demonstration techniques. It is also used as the base for groundwater field methods courses.

These tools include: 1) Electrical Resistivity Meter. The AGI SuperSting R8 IP is an 8-channel resistivity and induced polarization imaging system specially designed for large surveys where speed of data acquisition is of essence. Can be used for land applications with 6 m spacing, underwater applications with 2 m spacing, or boat-towed surveys with 1 to 5 m spacing. 2) Infrared Camera. The FLIR ThermaCAM SC640 is a high-resolution thermal infrared camera. The portable handheld radiometer (7.5 to 13 micron wavelength) takes images at 640x480 pixels at rates of down to 16 Hz. The precision of the camera is 0.08 C.

A 4' x 6' bench-top physical model simulating water flow under ice sheets and glaciers. Ice is represented by a transparent polymer. Water is injected below the "ice" at varying rates to observe the effects of discharge pulses on the channel geometry and surface motion of the "ice." Changes in discharge are designed to mimic a typical diurnal discharge pattern observed on alpine glaciers.

The IsoProbe MC-ICP-MS is a multicollector, magnetic-sector inductively coupled plasma mass spectrometer featuring a hexapole collision cell immediately behind the interface region of the ICP, and the multicollector contains nine Faraday collectors, three channeltron ion-counting detectors for low-level signals (ion currents below 10-16 amp), and an axial Daly detector located behind a wide aperature retarding potential filter for high abundance sensitivity on the Daly detector. The IsoProbe mass spectrometer is capable of making isotope ratio measurements in a large number of systems, including Ca, Fe, Cu, Se, Rb-Sr, Sm-Nd, Lu-Hf, Re, common Pb, Th-U series isotopes, and in situ laser ablation measurements of Sr, common Pb, Lu-Hf, and U-Pb.

The Isotope Clean Lab is a 600 square foot clean chemistry lab with seven Class-100 workspaces for preparation of rock, mineral, soil, plant and water samples for chemical and isotopic analysis under low-contamination conditions.

Custom built 5-m tilting flume. Width: 30 cm. Depth: 1 meter. Other features: 3 removable windows with septa ports, fluids can be extracted or injected from the floor.

Major instrumentation includes: (1) Gas chromatograph-single quadrupole mass spectrometer (GC-IRMS) for quantification and identification of organic compounds, and (2) HPLC-signgle quadrupole mass spectrometer (HPLC-MS) equipped with intelligent fraction collection for identification, quantification and isolation of high molecular weight compounds.

The REL includes a geoprobe for drilling, an Ion Chromatograph for analyzing anions and cations, and a stratified aquifer sampler for analyzing varying groundwater flow and quality with depth.

This lab is designed for the study of caves, soils and vegetative canopies. The GasBench II and Thermo Electron 253 in the High Temp. Stable Isotope lab are currently being used to measure the carbon isotope composition of soil and cave CO2, CO2 respired in soil respiration experiments, and dissolved inorganic carbon and calcium carbonates from multiple environments.

A GWR superconducting gravimeter (precision ~0.01 micrGals) configured to be transportable, used in hydrologic and other studies. This is usually deployed in the field for campaigns of months and longer.

The UTDW Basin is an experimental tank designed to physically model morphodynamic and stratigraphic evolution of continental margins and other subaqueous sediment transport systems. It is 4 m wide, 8 m long, and 2 m deep. The tank has 5 observation windows, underwater lighting and an array of synced overhead cameras. The facility is designed to map underwater deposit surfaces in space through time and measure fluid dynamic and sediment transport properties of formative density flows.

The STEP Basin is an experimental flume designed to physically model morphodynamic and stratigraphic evolution of the fluviodeltaic system. It is 4 m wide, 5 m long, and 1.5 m tall. This facility is one of only three in the world with a computer-controlled basement motion, which can mimic 1) fore-hinge (passive margin), 2) back-hinge (foreland basin), and 3) lateral tilting subsidence patterns.

The primary research collections of the library presently include more than 100,000 book and journal volumes and 46,000 geologic maps, among them the publications of the U.S. Geological Survey, most state geological surveys, and those of many foreign countries. Regional emphasis of the collection is on the Southwestern United States, Texas, and Mexico. The Institute and Bureau also have extensive libraries related to their specific research areas.

The Department of Geological Sciences maintains two wind tunnels for experiments in aeolian transport. One tunnel (0.5 m2 X 10 m) features a long transport section that ends in a slipface. The second tunnel features a rotating table (1 m in diameter) that can be used to simulate any range of wind directions.

The Center for Integrated Earth System Science (CIESS) is a cooperative effort between the Jackson School of Geosciences and the Cockrell School of Engineering. The center fosters collaborative study of Earth as a coupled system with focus on land, atmosphere, water, environment, and society.

The LEAD group consists of graduate research assistants, postdoctoral fellows, research scientists and visiting scholars. We view the earth system in a holistic way, linking the atmosphere, ocean, biosphere, cryosphere, and solid earth as an integrated system. We use powerful methodologies such as satellite remote sensing and supercomputing simulations which are now profoundly changing research in earth system sciences. We place a strong emphasis on the societal impact of the research in earth system sciences.

The University of Texas at Austin, Center for Space Research was established in 1981 under the direction of Dr. Byron D. Tapley. The mission of the Center is to conduct research in orbit determination, space geodesy, the Earth and its environment, exploration of the solar system, as well as expanding the scientific applications of space systems data.