The Southern Oklahoma aulacogen is a northwest-trending structure containing abundant igneous rocks representing the remains of a major Cambrian rift zone. Previous geologists have mapped numerous igneous intrusions in Colorado that follow the same trend, ranging from Ediacaran to Ordovician in age, and have speculated that these intrusions may be a part of the same rift. These intrusions include abundant igneous dikes of various compositions that originated from deeper magmatic bodies, filling fracture systems in older igneous rocks and Precambrian gneisses. This study involves the geochemical analysis of samples we collected from diabase dikes found along that northwest trend in southern Colorado. The dikes include a prominent diabase dike swarm in the Gunnison area as well as other individual dikes in the Wet Mountains and Front Range farther east. On the discrimination and REE diagrams, twenty-six representative dike samples from both sample regions plot tightly together, indicating the clustered dikes share a petrogenetic history of E-MORB-type magma that interacted with intercontinental lithosphere. In addition, this cluster generally plots within the same regions as data from diabase dikes associated with the Southern Oklahoma aulacogen.
Fifteen samples were taken from generally NW-trending diabase dikes in the Gunnison dike swarm, and these make up the majority of the dike samples that cluster together. The remaining eleven samples originate from general NW-trending diabase dikes in other locations across southern Colorado. Five samples were taken from WNW- to NW-trending diabase dikes in the Wet Mountains. Five samples were taken from NW- to NNW-trending diabase dikes in the Front Range, ~80 km north of the Wet Mountains. One sample was taken from a NW-trending diabase dike in the Unaweep Canyon, ~270 km west-northwest of the Wet Mountains.
The geochemical similarities between diabase dikes sampled for this study and those within the Southern Oklahoma aulacogen suggest a linked petrogenetic history. Furthermore, the distribution of these samples raises the intriguing possibility that dikes related to Ediacaran-Ordovician intraplate magmatism in Colorado may be more extensive than previously thought.

Landslides are a common and potentially destructive natural hazard, posing risks to infrastructure, ecosystems, and human populations. Central Texas, particularly Hill and Bosque Counties within the Texas Hill Country, is prone to landslide occurrence due to its rugged topography and variable geologic formations. This project assesses landslide susceptibility across the region using spatial analysis techniques in a GIS framework. Multiple datasets were integrated, including Digital Elevation Models (DEMs) to derive slope and flow accumulation, geologic formations, soils (hydrologic and erosion data), and stream networks. Each dataset was reclassified according to relative landslide risk and combined through a weighted overlay analysis to produce a landslide susceptibility map identifying areas of low, moderate, and high risk. The resulting map provides a framework for environmental hazard assessment and can support land-use planning and risk mitigation strategies in Central Texas.

The Visible Infrared Imaging Radiometer Suite (VIIRS) instrument onboard of the Suomi-NPP satellite has provided unprecedented night time light data that could be used as an indirect indicator of various parameters, including light pollution, population distribution, etc. The proposed project will integrate multi-temporal night light data from VIIRS with other datasets, including population data from the most recent census, ground-based light classification data (Bortle scale) to better understand how population growth affects light pollution over time, and to give insight into the importance of Dark Sky Preserves as population growth continues, across the State of Texas. Various spatial and statistical analysis techniques will be applied to address the objectives of this proposal including hotspot and density analyses, and statistical analysis of changes in population datasets.

The Fort Worth Nature Center (FWNC) is one of the largest city-owned nature centers in the U.S., located in northwest Tarrant County. It covers over 3,600 acres, including nearly 20 miles of hiking trails. The park is home to a wide variety of species within a diverse ecosystem that includes forests, prairies, and wetlands. Currently, there are multiple ongoing projects assessing invasive species, habitat management and restoration, and the impact of park visitors, among others. However, little has been done to understand the local hydrology, its dynamics across the park, and its interactions with watershed-scale processes, as well as the resulting impacts on refuge habitat. This project aims to integrate multiple spatial datasets and analysis tools, including digital elevation models (DEMs) and high-resolution hydrography datasets from the National Hydrography Dataset (NHD), to delineate hydrological features within the refuge, understand their dynamics, and assess their interactions with the medium and habitat within the refuge. The ultimate goal is to generate a product that can serve as input in FWNC’s efforts to monitor flood risk and support critical ecosystem and refuge planning.

This collaborative research project between Texas Christian University (TCU) Environmental Chemistry students and Texas Academy of Biomedical Sciences (TABS) AP Environmental Science students examines how physical characteristics- specifically thermal variation and bathymetric structure- influence water chemistry across the confluence of two river forks. Temperature is a critical abiotic factor in aquatic systems. As water temperature increases, the solubility of dissolved oxygen decreases favoring harmful algal blooms and stress in aquatic organisms. Variations in river depth and channel morphology influence flow dynamics, mixing processes, and habitat heterogeneity. By quantifying these physical drivers, this study provides insights into the spatial variability of water chemistry and contributes to a broader understanding of ecological processes within an urban river system.