#geomorphology

[grainelevator]

Faraway views (right lens of my binoculars)

[lake-lady]

[amethysthands]

Went on my first geomorph lab. Here are awesome examples of honeycomb weathering and natural pillars. I thoroughly enjoyed it !

[lowcountry-gothic]

Flame Azalea flashing their bright orange coloring against a lush green backdrop of North Carolina mountains underneath a blue sky of building clouds. Roan Highlands, Southern Appalachian Mountains. Carter, Tennessee. Photo by Mark van Dyke.

[bettergeology]

Mementos from the Zabriskie badlands, Death Valley NP, California

What happened here? Well, I’ll tell you:

Death Valley is a huge tectonic basin. That is, it was formed by plate tectonics rather than erosion from water. It is not the first valley here, however. Valleys and basins are recorded in Death Valley’s rock record several times in the last ~25 million or so years, culminating in the current huge valley which is the deepest point below sea level in the western hemisphere. At Golden Canyon, a popular easy hiking spot, the rocks record previous editions of Death Valley. Called the Furnace Creek Formation, these soft yellow-brown rocks are made of lake sediments that were laid down when an older, smaller basin existed about 3-5 million years ago. In places, minerals in these rocks mark times when that lake dried up, recording a climate history of the area!

Less than a million years after this rock sequence was laid down, the very active faults on either side of it tore this basin apart. The rocks were folded, faulted, tilted, and uplifted to their current position by the Northern Death Valley fault and the Black Mountains faults. Slowly, the soft rocks eroded down to reveal their story, now visited by about one million people per year.

[mesetacadre]

this massive fault in Spain's Central System is gorgeous and underdiscussed. They even have a road running through the middle...

[eopederson]

Cirques, Central Colorado Rockies from IAD-LAX Flight, 2023.

The evidence for extensive glaciation is ample in the Colorado Rockies.

[historysurvivalguide]

Science Science-Fiction Movies

Not all scientists are physicists! Here are some movies that highlight different fields of study

All fully recommended, some of my personal favorites

Geomorphology and Geophysics: The Core

Geomorphology: the scientific study of the physical and chemical processes that impact how surface of a planet changes. For example, a fluvial geomorphologist is a scientist that studies how rivers (fluvial) change the surface of a planet. Not always Earth, some geomorphologist study planets like Mars and Mercury. Earth science is more than just geology and rocks! Sometimes it also about rocks moving around or being eroded 🌏

Meteorology: Twister and Twisters

Meteorology: the study of a planet’s atmosphere with a strong focus on forecasting the weather 🌪️

Linguistics: The Arrival

Linguistics: the scientific study of languages 🖋️

Seismology: Tremors

Seismology: the scientific study of earthquakes 🪇🪨

Heliophysics and Solar Physics: Sunshine

Heliophysics: the scientific study of the sun and its effects on the solar system ☀️

Paleontology: Jurassic Park

Paleontology: the scientific study of life on earth through the fossil record 🦴 🦕

Botany and Astrophysics: The Martian

This one is a bit of a mix. The book makes uses of a lot of astrophysics, but the character is a botanist

Astrophysics: the scientific study of physical and chemical processes of the cosmos (a newer field of astronomy that includes more of a focus on physics) 🛰️

Botany: the scientific study of plants 🌱

Genetics and Astronomy: Gattaca

Another mix! The main theme of the movie revolves around genetics and genetic engineering (specifically eugenics). However, the main character is an astronomer/astronaut

Genetics: a branch of biology that concerns the scientific study of genes, genetic variation, and heredity 🧬

Astronomy: the study of space, stars, planets, and other celestial objects 🪐

[noosphe-re]

Geomorphology is the study of the form of the earth. Coastal geomorphologists study the way that the coastal zone, one of the most dynamic and changeable parts of the earth, evolves, including its profile, plan-form, and the architecture of foreshore, backshore, and nearshore rock and sediment bodies. To understand these it is necessary to examine wave processes and current action, but it may also involve drainage basins that feed to the coast, and the shallow continental shelves which modify oceanographic processes before they impinge upon the shore. Morphodynamics, study of the mutual co-adjustment of form and process, leads to development of conceptual, physical, mathematical, and simulation models, which may help explain the changes that are experienced on the coast.

C. Woodroffe, Geomorphology, in Encyclopedia of Ocean Sciences, 2001

[trolledu]

A new ocean is slowly forming in Africa due to a 35-mile crack that appeared in Ethiopia in 2005. This crack is caused by three tectonic plates—the Nubian, Somali, and Arabian plates—gradually pulling apart. Scientists estimate it will take 5 to 10 million years for the ocean to fully form.

The Afar region, where the plates meet, is a unique place to study tectonic processes. Some researchers believe the rift is driven by a massive plume of superheated rock rising from the Earth’s mantle beneath East Africa. The plates are moving at different speeds, with the Arabian plate drifting away from Africa at about 1 inch per year and the African plates separating even slower, between 0.2 to 0.5 inches annually.

Eventually, this process will create a new mid-ocean ridge system, paving the way for a new ocean to emerge in Africa.

[dissolveyourfilter]

Bryce hike!

[grainelevator]

The aeolian processes of katabatic winds in Antarctica’s McMurdo Dry Valleys shape boulders into surreal formations

[happy-little-letters]

Quaternary Geomorphology

I became a surficial mapper this summer, following the step-cuts of proglacial shorelines across farm fields and verdant aspen stands, until the ghost of water took form. There lies the joy of geomorphology, vivid and visible, screaming out a story once you learn how to look for its traces.

I think love leaves traces.

This fall, I am taking dance lessons in the basement of my students' union. My instructor has the same cupid's bow smile of someone I once kissed, who talked me through the top surgery referral process one spring-green evening. I am wearing hand-me-down flannel from a friend half a continent away. Oh, friendly ghosts, hello -- I dance with a girl with field-rough hands and recognize the heat blooming beneath my ribs as my constant. We are caught in the process of becoming, all. Nothing, love nor learning, is ever wasted. It is only transformed, lakeshore clay to loam.

Look, you can see it still.

[basicgeology]

Knickpoints, base level, and waterfalls

I won't go into detail about hydraulics, but hi! Let's talk about rivers a little!

Base level: in geomorphology, the "base level" is the lowest point at which erosion can occur, or in the case of rivers, it's the lowest altitude at which a river can flow. A common base level for most rivers is the sea, though for some of them it might be a lake, a different river that the first river is a tributary to, or a dam.

The base level for any given river can change through time, since sea levels can vary, dams can be built, etc. A variation in base level, causes a variation in the river's energy, which can lead to more erosion, or more sediment deposition depending on if the river has more or less energy than before.

Here are two examples, the first is of a river whose base level dropped lower, it gained more energy and started eroding the substrate more, the second one is of a river whose base level was raised higher, and it started depositing more sediment to compensare with lowered energy.

This was an introduction to explain the concept of base level, now let's move on to knickpoints.

Knickpoint: a sudden and sharp variation of a river's slope, often leading to the formation of waterfalls and/or lakes. Some reasons why a knickpoint might form are: base level drop, tectonic activity, or a later of erosionally resistant rock:

There are generally two types of knickpoints: migrating and fixed.

Migrating knickpoints are mainly caused by base level drop and tectonic activity. They are called migrating because due to the erosion that the river applies on the substrate, the knickpoint is able to travel upstream. In the case of a base level drop type of knickpoint that affects an entire hydrography basins, usually the baisin will have all of its migrating knickpoints at the same altitude:

Sometimes, knickpoints are caused by differential uplift (two areas within a hydrographic basin are subject to different rates of tectonic uplift), and this causes a "barrier" of knickpoints that can easily be drawn within the baisin:

Fixed knickpoints instead are caused mostly by the presence of a layer of erosionally resistant rock, as it is something that the river cannot easily erode through, and will remain fixed.

Waterfalls can form from any of these kinds of knickpoints, it really depends on the river's erosion ability, it's energy, it's mass flow rate, the kind of sediments it carries, etc.

[lowcountry-gothic]

Blue Ridge Parkway in North Carolina.

[braidedriver24]

some impressions of my field trip to the havel river in brandenburg / germany some weeks ago

we worked on an island between the channels of the river which had sometimes a quite swampy environment (the bright green parts of the landscape are actually bit lower and are former channels of the havel). luckily i didn't forget to bring my rubber boots (please admire the flower print, my local shoe shop didn't had my size so i had to choose between them or one pair with a paw patrol print). we also took some core samples from the island and the surrounding lakes which was really fun and did some geophysical surveys. at the last day we visited a hill fort from the slavic medieval times which was really impressive