Graduate positions at Boise State University

The cryosphere research program at Boise State University is looking for 3 graduate students to conduct research on mountain snow and glaciers as part of an interdisciplinary NASA EPSCoR program that will begin winter 2021. The students will work closely with several faculty at Boise State as well as faculty at the University of Idaho to quantify and model variation in snow accumulation and melt in mountainous and glacierized terrain. We seek students that will align with one of three potential subject areas:

Quantify the impact of topography and vegetation on the distribution of seasonal snow, and its impact on snowmelt timing.

Improve empirical and numerical models of snow accumulation and snow and ice melt in mountain regions using ICESat-2 observations.

Develop a workflow to design sparse, efficient in-situ observational networks to minimize uncertainties in basin-scale meltwater flux estimates from remotely sensed and modeled data.

Additional funded graduate projects focused on the application of a variety of geophysical methods to measure mountain snowpack and associated hazards will soon be available as well. Details on these additional positions will be posted at https://www.boisestate.edu/earth-cryogars/.

We seek students with broad backgrounds to engage in collaborative, interdisciplinary research while completing degrees in Geophysics, Geoscience, Hydrology, or Scientific Computing. The professional development of students will be supported through a variety of research and engagement activities. These include opportunities to design and conduct field investigations in Idaho and Alaska and gain formal and informal training in science education. The interdisciplinary scientists trained through participation in this project will be provided with the resources and connections needed to meet their professional goals.

Three year fully-funded student positions are available starting as early as January 2021, so applications will be evaluated as they are received. We welcome and encourage applicants with backgrounds historically underrepresented in STEM and Earth Sciences. Note that graduate programs in the Department of Geosciences at Boise State do not require or consider GRE scores in admissions. Check out the Boise State Graduate College, as well as the Department of Geosciences and PhD in Computing program websites, for information about the university and graduate degree programs.

Please contact Dr. Ellyn Enderlin (ellynenderlin@boisestate.edu) for more information about the available positions and/or to set-up an informal remote interview. Additional information about the Enderlin Glaciology Group can also be found at https://sites.google.com/site/ellynenderlin/home.

....

Vineesh V
Assistant Professor of Geography,
Directorate of Education,
Government of Kerala.
https://www.facebook.com/Applied.Geography
http://geogisgeo.blogspot.com
🌏🌎
🌐🌍

Comments

Geologic and tectonic framework of the Indian shield

Major Terms and Regions Explained 1. Indian Shield The Indian Shield refers to the ancient, stable core of the Indian Plate made of hard crystalline rocks. It comprises Archean to Proterozoic rocks that have remained tectonically stable over billions of years. Important Geological Features and Regions ▪️ Ch – Chhattisgarh Basin A sedimentary basin part of the Bastar Craton . Contains rocks of Proterozoic age , mainly sedimentary. Important for understanding the evolution of central India. ▪️ CIS – Central Indian Shear Zone A major tectonic shear zone , separating the Bundelkhand and Bastar cratons . It records intense deformation and metamorphism . Acts as a suture zone , marking ancient tectonic collisions. ▪️ GR – Godavari Rift A rift valley formed due to stretching and thinning of the Earth's crust. Associated with sedimentary basins and hydrocarbon resources . ▪️ M – Madras Block An Archean crustal block in...

Geology and Tectonic. Indian Shield

1. Ch (Chattisgarh Basin): Chattisgarh Basin is a geological region in central India known for its sedimentary rock formations. It's important for its mineral resources, including coal and iron ore. 2. CIS (Central Indian Shear Zone): CIS is a tectonic boundary in central India where the Indian Plate interacts with the Eurasian Plate. It's characterized by significant faulting and seismic activity. 3. GR (Godavari Rift): The Godavari Rift is a geological feature associated with the rifting and splitting of the Indian Plate. It's located in the Godavari River basin in southeastern India. 4. M (Madras Block): The Madras Block is a stable continental block in southern India. It's part of the Indian Plate and is not associated with active tectonic processes. 5. Mk (Malanjkhand): Malanjkhand is known for its copper deposits and is one of the largest copper mines in India. 6. MR (Mahanadi Rift): The Mahanadi Rift is a geological feature related to the rifting of the Indian Pl...

Evaluation and Characteristics of Himalayas

Time Period Event / Process Geological Evidence Key Terms & Concepts Late Precambrian – Palaeozoic (>541 Ma – ~250 Ma) India part of Gondwana , north bordered by Cimmerian Superterranes, separated from Eurasia by Paleo-Tethys Ocean . Pan-African granitic intrusions (~500 Ma), unconformity between Ordovician conglomerates & Cambrian sediments. Gondwana, Paleo-Tethys Ocean, Pan-African orogeny, unconformity, granitic intrusions, Cimmerian Superterranes. Early Carboniferous – Early Permian (~359 – 272 Ma) Rifting between India & Cimmerian Superterranes → Neotethys Ocean formation. Rift-related sediments, passive margin sequences. Rifting, Neotethys Ocean, passive continental margin. Norian (210 Ma) – Callovian (160–155 Ma) Gondwana split into East & West; India part of East Gondwana with Australia & Antarctica. Rift basins, oceanic crust formation. Continental breakup, East Gondwana, West Gondwana, oceanic crust. Early Cretaceous (130–125 Ma) India broke fr...

Seismicity and Earthquakes, Isostasy and Gravity

1. Seismicity and Earthquakes in the Indian Subcontinent Key Concept: Seismicity Definition : The occurrence, frequency, and magnitude of earthquakes in a region. In India, seismicity is high due to active tectonic processes . Plate Tectonics 🌏 Indian Plate : Moves northward at about 5 cm/year. Collision with Eurasian Plate : Causes intense crustal deformation , mountain building (Himalayas), and earthquakes. This is an example of a continental-continental collision zone . Seismic Zones of India Classified into Zone II, III, IV, V (Bureau of Indian Standards, BIS). Zone V = highest hazard (e.g., Himalayas, Northeast India). Zone II = lowest hazard (e.g., parts of peninsular India). Earthquake Hazards ⚠️ Himalayas: prone to large shallow-focus earthquakes due to active thrust faulting. Northeast India: complex subduction and strike-slip faults . Examples: 1897 Shillong Earthquake (Magnitude ~8.1) 1950 Assam–Tib...

Vector geoprocessing - Clipping, Erase, identify, Union & Intersection

Think of your vector data (points, lines, polygons) like shapes drawn on a transparent sheet. Geoprocessing is just cutting, joining, or comparing those shapes to get new shapes or information. 1. Clipping ✂️ Imagine you have a big map and you only want to keep a part of it (like cutting a photo into a smaller rectangle). You use another shape (like the boundary of a district) to "clip" and keep only what is inside. Result: Only the data inside the clipping shape remains. 2. Erase 🚫 Opposite of clipping. You remove (erase) the area of one shape from another shape. Example: You have a city map and want to remove all the park areas from it. 3. Identify 🔍 This checks which features from one layer fall inside (or touch) another layer. Example: Identify all the schools inside a flood zone. 4. Union 🤝 Combines two shapes together and keeps everything from both. Works like stacking two transparent sheets and redrawing t...

Vineesh V, Geography

Search This Blog