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Celebrating Geoscience Week: A Journey into the Earth’s Mysteries

When is Geoscience Week?

Geoscience Week is an annual celebration that typically takes place in mid-October, aligning with Earth Science Week, a worldwide event. This year, Geoscience Week falls between October 13-21, bringing together professionals, students, and enthusiasts alike to explore the wonders of our planet. During this time, various organizations, schools, and institutions host activities, workshops, and outreach efforts designed to raise awareness about the earth sciences and their vital role in society.

What is Geoscience Week?

Geoscience Week shines a spotlight on the diverse disciplines within earth sciences, such as geology, meteorology, oceanography, and environmental science. Geoscientists investigate Earth's processes—like the formation of mountains, the behavior of oceans, or the dynamics of climate—and the ways in which these processes impact human life and the environment. This week aims to inspire a deeper appreciation for our planet’s natural systems and highlights the scientific advancements that allow us to sustainably interact with them.


From studying earthquakes and volcanoes to mapping mineral resources and understanding water cycles, geoscientists play an integral role in how we explore, manage, and protect our world. Geoscience Week invites the general public to discover these subjects through accessible events such as nature walks, public lectures, interactive exhibits, and online educational campaigns.

Why is Geoscience Week Important?

  1. Understanding Our Planet's Past, Present, and Future
    Geoscientists provide crucial insights into Earth's history through the study of fossils, rocks, and minerals. This knowledge helps us understand past climate patterns, natural disasters, and even the origins of life itself. By grasping Earth’s historical context, we can better prepare for future challenges like climate change, resource depletion, and environmental hazards.
  2. Sustainable Resource Management
    Earth provides the raw materials that fuel our economy—whether it’s the oil and gas that powers our cars or the minerals used in our smartphones. Geoscience ensures that we can extract and use these resources in ways that minimize environmental damage. As society pushes for a greener, more sustainable future, geoscientists are essential in the search for alternative energy sources, such as geothermal power, and in managing the impact of industrial activities on the environment.
  3. Mitigating Natural Disasters
    Earthquakes, landslides, tsunamis, and volcanic eruptions are natural processes that can devastate communities. Geoscientists study these phenomena to predict when and where they may occur, potentially saving countless lives through early warning systems and improved disaster preparedness. Their work also aids in developing strategies to minimize the impacts of these events on infrastructure and society.
  4. Promoting Environmental Stewardship
    Geoscience Week reminds us that we are custodians of the planet. As issues like climate change, pollution, and deforestation take center stage, geoscientists are at the forefront of researching and implementing ways to protect Earth's ecosystems. Their efforts guide conservation practices and policies, helping to preserve biodiversity and sustain vital natural resources for future generations.


Why Should You Get Involved?

By participating in Geoscience Week, you’ll gain a greater appreciation for the natural world and the critical role geoscientists play in our daily lives. Whether you attend a local event, join an online discussion, or simply share educational content, you’ll contribute to the growing awareness of geoscience’s importance in shaping a sustainable future. The more we understand our planet, the better equipped we are to protect it for generations to come.



This Geoscience Week, take a moment to celebrate the dynamic forces that have shaped Earth over billions of years—and the scientists who dedicate their careers to studying it. Every rock, river, and ripple tells a story, and geoscientists are here to decode them for the benefit of all.

By Andrew J. Davidoff, Ph.D., P.G. November 8, 2024
Case Summary One of the first things an oil and gas company must do before they can drill a well is to obtain the mineral rights for the land they want to drill on. The most common way to do this is to lease the mineral rights to the land. These leases come with certain unwritten legal or hidden obligations, known in the legal world as “implied covenants.” Oil and gas leases contain several implied covenants. One of them is known as the “Duty to Develop.” This refers to the obligation of an Oil and Gas Company (the lessee) to make reasonable efforts to explore and develop an oil and gas lease. Whether or not an oil and gas company has lived up to its obligation to develop a lease responsibly may become a matter of dispute and sometimes ends up in the courts. Understanding the subsurface geology is often critical in determining whether a company has met its obligations. The question often comes down to whether a company can profit from additional drilling or other development activities. Answering this question is, at least in part, frequently dependent upon the potential quantity of oil and/or gas in the subsurface. These questions require the expertise of geologists and often additional subsurface professionals such as geophysicists, petrophysicists, reservoir engineers, and others. The following provides an example in which an operator was found to have breached their obligations to make reasonable efforts to explore and develop oil and gas in a lease and the role geology played in the case. The case went to court in the 1980s, but its origins can be traced back to the 1930s when a major oil and gas company leased a 10,000-acre tract of land along the onshore Texas Gulf Coast. The company used seismic reflection technology to explore for oil and gas on the lease. The use of seismic reflection data in oil and gas exploration is common and standard operating procedure today, but in the 1930’s, it was leading-edge technology. The use of seismic enabled the discovery of oil and gas in a sandstone layer in a rock unit called the Frio Formation. The discovery was made in the early 1940s. Over the next decade, the company found three more oil and gas-bearing sandstone layers in the Frio Formation. By the time the case went to trial, the company had drilled 64 wells and acquired an additional 13 seismic surveys. The field covered an area of over 1,100 acres. It had produced over 100 million barrels of oil, over 100 billion cubic feet of gas, and over 50,000 barrels of condensate, with royalties providing an average income of $10,000 per day. At the time of the trial, 37 wells were still producing. However, the remaining 8,900 acres of the 10,000-acre remained unexplored and undeveloped. Fields along the Texas Gulf Coast were also known to produce hydrocarbons from slightly deeper and older sandstones in the Vicksburg Formation. The case hinged on the question of whether the operator had fulfilled its obligation to explore the remaining 8,900 acres and test the potential of the Vicksburg Formation. Expert Analysis The Operator claimed there was only one structure and one formation with sufficient porosity and permeability to trap and produce hydrocarbons. The landowner (the lessor) challenged this claim and hired a geologist to review the subsurface data. The geologist for the lessor reviewed the data across the field and concluded that the remaining 8,900 acres of land could contain additional oil and gas accumulations. They also concluded that oil could be present not only in sandstones of the Frio Formation but also in a deeper formation called the Vicksburg. The jury was tasked with determining whether the Oil and Gas Company had acted reasonably in exploring and developing the lease. The answer to this question required the jury to learn about the geology in the area, how the oil and gas became trapped in the rocks, and the tools used by geologists and geophysics to understand the subsurface. The subsurface along the Texas Gulf Coast is dominated by sandstones and shales deposited by ancient rivers and in deltas, beaches, barrier islands, and marshes. The sandstones form porous and permeable layers that can both store oil and gas and through which oil and gas can move or migrate. These layers are often called reservoir rocks. Shales form impermeable layers through which oil and gas cannot move, often called seals. Oil fields are formed when reservoir rocks, seals, and subsurface structures combine in such a way as to create a feature (called a trap) into which oil can migrate and be stored for 10s and even 100s of millions of years. There are many different types of traps in which hydrocarbons can accumulate. One of the most common is the anticline. An anticline resembles a hill or an inverted bowl. Oil or gas will migrate upward through porous rocks and become trapped at the crest of the anticline (Figure 1a). The oil industry aims to find hydrocarbons trapped in the subsurface that can be produced at a profit. To do this, the oil and gas industry collects and analyses vast quantities of subsurface geologic and geophysical data. These data are divided into two broad categories: well data and seismic data. [1] Well data is information collected from the well bore, that is the hole in the ground created by the drilling process. The data may be collected while the well is drilling or shortly thereafter. Data typically collected and used by the geologist includes mud logs, well logs, and core. Mud logs: When drilling a well, fluid is used to cool the bit and carry rock fragments created by the drilling process away from the bit and to the surface. This fluid is called “mud”. Modern mud logs record the lithology of the drilled rocks based on the rock fragments and the presence of oil and gas carried to the surface by the mud. Well Logs : These are measurements of the rock properties inside the well bore. A few of the most common measurements used today include natural gamma radiation, resistivity, density, and neutron porosity. These measurements are made after the well has been drilled. Sophisticated tools are lowered to the bottom of the well. Rock property measurements are made as the tools are pulled out of the well. Core: These are samples of the rock taken either during drilling. Whole-diameter cores are taken by replacing the drill bit with a special coring tool. The tool allows cylinders of rock to be retrieved from the subsurface. Seismic data collected by the oil and gas industry uses sound waves to create an image of the subsurface, similar to how doctors use ultrasound to create images of a baby in a mother's womb. The process starts by sending vibrations through the earth. In the past, dynamite was used to generate vibrations and is still used in some places. Today, trucks that vibrate the ground are more common. The sound waves travel through the earth and are reflected from rock layers and other places where the rock properties change. Sensitive listening devices called geophones onshore record these reflections. The reflections are used to create images of the rocks in the subsurface. One important thing to know about seismic data is that it records the time it takes for the sound waves to travel down through the earth and reflect back to the geophone. These times must be converted to depth to generate maps, cross sections, and drilling prognosis. The data collected and used to analyze the field discussed here was extremely primate compared to modern data. At the time of discovery, all the data collected across the field, including well-log and seismic data, was based on analog technology. Geophysicists had to calculate by hand the time it took for each reflection to travel down and back and then convert that to depth. When this case went to trial in the 1980s, technology had advanced significantly since the time of discovery but it was still primitive compared to what we see today. Well logs were printed on folding paper a foot wide and tens of feet long. Interpretation was typically done by hanging the logs on walls or laying them out on drafting tables so the sand layers and formation boundaries could be correlated from well to well using colored pencils. [1] The purpose of this article is only to provide an example of some of the data types used by the oil and gas industry. The data types presented here have therefore been limited.
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