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Grizzly bears removed for livestock depredations

Grizzly bears removed for livestock depredations

Grizzly bears removed for livestock depredations. Two grizzly bears were removed last month due to cattle depredations in southwestern Montana.

One bear was killed in the Gravelly Mountains after several instances of sheep depredation. These conflicts happened despite multiple attempts to avoid them, including guard dogs, moving sheep to new areas, and hazing the bear.

The second bear was killed on private land in the Paradise Valley south of Livingston after chronic cattle depredations. The landowner moved cows twice, but conflicts continued.

The U.S. Department of Agriculture’s Wildlife Services removed both bears on Aug. 21 in consultation with the U.S. Fish & Wildlife Service and Montana Fish, Wildlife & Parks.

Specialists with FWP and Wildlife Services work to help landowners, producers and communities avoid bear conflicts. Promptly reporting bear conflicts can make a difference for the health of the bear and the safety of communities. Some corrective management efforts, when applied early, can be effective in discouraging bears from being close to humans and livestock and reduce future conflicts.

To report bear conflicts, contact your local bear specialist at the phone number listed on FWP’s website: https://fwp.mt.gov/conservation/wildlife-management/bear/contact.

FWP Guidance for Livestock Owners, Homeowners and the General Public

“Grizzly bears are listed as Threatened under the Endangered Species Act (ESA). As such, harassing, harming, pursuing, hunting, shooting, wounding, killing, trapping, capturing, or collecting grizzly bears is not permitted except for self-defense or in defense of others, as authorized by the grizzly bear 4(d) rule. Harass in the definition of “take” in the ESA means an intentional or negligent act or omission which creates the likelihood of injury to wildlife by annoying it to such an extent as to significantly disrupt normal behavioral patterns which include, but are not limited to, breeding, feeding, or sheltering.”

“Grizzly bears can pose a threat to human safety and should be discouraged from using areas near homes and other human-occupied areas. Hazing discourages undesirable behavior in wildlife, and when properly conducted, does not create a likelihood of injury to grizzly bears to such an extent as to significantly disrupt normal behavioral patterns.”FWP Guidance Report

sourced – Montana Fish, Wildlife & Parks – Sep 11, 2024




 

Why do Heat Index and Wind Chill temperatures exist?

Why do Heat Index and Wind Chill temperatures exist

Why do Heat Index and Wind Chill temperatures exist? Heat index and wind chill temperatures exist to provide a more accurate representation of how weather conditions feel to the human body, rather than just the actual air temperature.

Here’s why each is important:

Heat Index:

The heat index, also known as the “apparent temperature” or “feels like” temperature, measures how hot it really feels when humidity is factored in with the actual air temperature.

High humidity reduces the rate at which sweat evaporates from the skin, which is the body’s primary cooling mechanism. When sweat doesn’t evaporate as quickly, the body retains more heat, making the environment feel hotter than it actually is. This can lead to heat-related illnesses like heat cramps, heat exhaustion, or heat stroke.

The heat index also helps in predicting the risk of heat stress, especially for outdoor workers, athletes, and anyone spending time outside in hot, humid conditions.

Wind Chill:

Wind chill temperature indicates how cold it feels on exposed skin due to the wind. It’s based on the rate of heat loss from the body surface.

Wind speeds up heat loss from the body. When the wind blows, it can carry away the thin layer of warmed air around your body, making you feel colder much quicker than the actual air temperature would suggest. This can lead to frostbite or hypothermia in extreme conditions.

Wind chill is crucial for warning people about the dangers of cold weather, particularly in winter sports, outdoor activities, or emergency situations. It helps in deciding appropriate clothing and precautions to prevent cold-related injuries.

Both indices are essential for public health and safety, providing a more realistic assessment of environmental conditions that affect human comfort and health.

These indices also help in informing people to take necessary precautions like hydration, appropriate clothing, or seeking shelter, also in assisting in scheduling outdoor activities or events at safer times.

Heat index and wind chill also assist with helping to prepare for and to respond to weather-related emergencies more effectively.

By understanding these indices, individuals and authorities can better prepare for and mitigate the risks associated with extreme weather conditions.

The next time you find yourself asking “Why do Heat Index and Wind Chill temperatures exist?” just remember what you’ve read here.

Thanks for the read.

Happy Trails
 




 

Plate Tectonics: The Shanxi Rift System

Plate Tectonics: The Shanxi Rift System

Plate Tectonics: The Shanxi Rift System, also known as the Fen–Wei Rift System, is a significant geological feature in northern China, forming the eastern margin of the Ordos Block.

Geographical Extent:

This rift system stretches over approximately 600 miles from the Qinling orogenic belt in the south to the Yinshan-Yanshan orogenic belt in the north. It varies in width from 25 to 75 miles.

See video:
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Tectonic Activity:

The system is characterized by active extensional tectonics, which means the crust is being pulled apart, leading to the formation of rift basins. These basins are arranged in an echelon pattern, indicating a complex interplay of tectonic forces.

Major Basins:

Weihe Basin: Known for its half-graben geometry, it thickens southwards with large normal faults defining its southern boundary against the Qinling Mountains.

Sanmenxia Basin: Located between the Qinling orogenic belt and the Zhongtiao Mountains, it shares a geological history with the Weihe Basin, featuring sedimentary rocks from the Eocene period.

Linfen Basin: Situated north of the Yuncheng Basin, it’s controlled by the Louyunshan Fault on its northwest side.

Geological History:

The initiation of the rift system is traced back to the Eocene period (about 50-35 million years ago), possibly triggered by the subduction of the Izanagi-Pacific ridge. It experienced reactivation around 8 million years ago, influenced by the India-Eurasia collision and the eastward extrusion of South China.

Current Interest and Research:

Discussions on social media and various online articles have highlighted the Shanxi Rift System for its geological wonder, particularly the rift valley in Pinglu, Shanxi. This area, part of the Loess Plateau, showcases dramatic geological features formed by crustal movements, attracting attention for its scenic beauty and geological significance.

Cultural and Scientific Impact:

While primarily a geological feature, the Shanxi Rift System’s influence extends into cultural aspects, as seen in references in video games like “Black Myth: Wukong,” indicating its integration into broader cultural narratives.

Environmental and Tourism Aspect:

The scenic beauty of areas like the rift valley in Pinglu has been highlighted around the internet, suggesting a growing interest in geological tourism. This could imply efforts towards conservation, education on geological processes, or simply appreciation of natural landscapes.

The Shanxi Rift System, therefore, not only represents a crucial area for understanding tectonic processes in China but also serves as a point of interest for cultural, environmental, and touristic activities. Its study continues to evolve, providing insights into Earth’s dynamic crustal movements and their implications on the landscape and human culture.

photo credit – Tuhaf Ama Gerçek (Plate Tectonics: The Shanxi Rift System)




 

Going-to-the-Sun Road closing Wednesday night

Going-to-the-Sun Road

Going-to-the-Sun Road closing Wednesday night: The alpine section of Going-to-the-Sun Road in Glacier National Park is scheduled to close at 9 p.m. on Wednesday, September 11, 2024, due to forecasted weather conditions that could lead to hazardous situations like mudslides and falling rock.

This closure will affect the stretch between Avalanche Creek and Jackson Glacier Overlook and is expected to last through the early morning of Friday, September 13, 2024.

Park officials are taking this precautionary measure in response to predictions of moderate to heavy rain showers and thunderstorms, which could make travel unsafe.

Visitors are advised to check the park’s road status and weather updates before planning their visit during this period.

You can learn more about this closure by visiting:
https://www.nps.gov/glac/learn/news/alpine-section-of-going-to-the-sun-road-closing-at-9-pm-tonight-due-to-storm-warning.htm

Note:

Going-to-the-Sun Road in Glacier National Park, Montana, is renowned for its scenic beauty, offering a drive through the heart of the Rocky Mountains with breathtaking views at every turn.

It’s length is approximately 50 miles long, stretching across Glacier National Park from west to east.

The elevation of the road reaches its highest point at Logan Pass, at 6,646 feet.

Travel time without stops, takes about 2 hours to drive the full length, but most visitors spend much longer to enjoy the views and amenities along the way.

There are restrictions on vehicle size due to the narrow and winding nature of the road, especially around Logan Pass.

Vehicles longer than 21 feet or wider than 8 feet are prohibited between Avalanche Creek and Rising Sun.

There’s a usually a partial closure to bicycle use between 3 pm and 6 pm from May 24th through September 8th. This is primarily aimed at managing traffic flow during peak times.

The road’s name comes from Going-to-the-Sun Mountain, reflecting both geological and cultural significance, especially from the Blackfeet tribe’s perspective, who have historical ties to the area.




 

Crispy Roasted Potatoes

Crispy Roasted Potatoes

Here’s a simple recipe for crispy roasted potatoes.

Ingredients:

2 lbs of potatoes (Yukon Gold or Russet work well)
3-4 tablespoons of olive oil or duck fat for extra crispiness
Salt, to taste
Black pepper, to taste
Optional seasonings:
2 teaspoons of rosemary or thyme (fresh or dried)
4 cloves of garlic, minced
1 teaspoon of paprika or smoked paprika

Directions:

Preheat Oven:

Preheat your oven to 425°F. If you have a convection setting, use it for even crispier potatoes.

Prepare Potatoes:

Wash the potatoes thoroughly. You can peel them or leave the skins on for extra texture.
Cut the potatoes into 1-inch cubes or wedges.

Parboil (optional but recommended for extra crispiness):

Place the potatoes in a large pot and cover with cold water. Add a generous pinch of salt.
Bring to a boil and cook for about 5-7 minutes. You want them to be slightly tender but not fully cooked.
Drain the potatoes and give them a good shake in the colander or pot to rough up the edges. This step is key for crispiness.

Seasoning:

Return the potatoes to the pot or transfer to a bowl.
Drizzle with olive oil or melted duck fat.
Add salt, pepper, and any optional seasonings you like. Toss well to coat evenly.

Roasting:

Spread the potatoes out in a single layer on a baking sheet lined with parchment paper for easier cleanup. Ensure they’re not too crowded; use two sheets if necessary.
Roast in the preheated oven for about 30-45 minutes, turning them halfway through with a spatula to ensure even browning.

Check to see if done:

They’re done when they’re golden brown and crispy on the outside, and you can easily pierce them with a fork.

Serve:

Optionally, sprinkle with a bit more salt or fresh herbs like parsley before serving.

Enjoy your crispy roasted potatoes as a side dish with your favorite main course, or even as a snack with a dip like garlic aioli or ketchup!