How Far Is 25km In Miles

How Far Is 25km In Miles – After walking the usual migration route from Red Desert to Hoback Junction near Jackson, Mule Deer Doe #255 continued on to Island Park, Idaho, traveling a total distance of 242 miles. That’s 92 miles beyond the longest known deer migration route. All summer, scientists waited to see if they would return or if they would just join another herd.

“But then in the first week of August, her collar failed,” said Matt Kauffman, director of the Wyoming Migration Initiative. “She just got lost.”

How Far Is 25km In Miles

But a year and a half later, she was found again at her winter residence, proving that the trip was a true migration.

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“My student has so often listened to deer no. 255 that she remembered the serial number on the necklace. She looked at the necklace, read the serial number and immediately knew it was Jelen #255. That was really exciting,” Kauffman said.

“She looks like any other doe from the outside,” Wyoming Game and Fish Department biologist Mark Zornes said with a laugh.

Zornes told Srna no. 255 is now migrating somewhere between Steamboat Mountain and Highway 28, but this time she is pregnant with sables.

“The interesting question is whether she will give birth to a fawn and whether she will successfully raise it and bring it home to the Red Desert for the winter and maybe pass on that trait that she clearly has?” Zornes said.

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To hear an interview with Matt Kauffman telling the full story of Jelen #255, listen to this week’s episode of Open Spaces.

Melodie Edwards is the host and producer of WPM’s award-winning podcast The Modern West. Her series Ghost Town(ing) looks at rural despair and resilience through the lens of her hometown of Walden, Colorado. She has been a radio reporter at WPM since 2013, covering topics from wildlife to American Indians to agriculture.”General Fremont’s Army Crosses the North Fork of the Shenandoah at Mt. Jackson–The Quest for Stonewall Jackson” by Edwin Forbes, 1862

While American Major General George B. McClellan advanced on Richmond with 100,000 troops, Confederate Major General “Stonewall” Jackson had orders for a strategic diversion in the Shenandoah Valley. In March 1862, he marched his small army of about 3,500 men north of Mount Jackson, determined to strike at the Federals.

Using aggressive tactics and a thorough knowledge of the Valley’s terrain, Jackson fought and defeated several Federal commanders in the Valley from late March to early June. A federal retreat in June allowed Jackson’s army to leave the valley on June 17 and join General Robert E. Lee’s beleaguered army near Richmond, the Confederate capital.

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Jackson heads for Staunton. Major General Richard S. Ewell’s Confederate division crosses the Blue Ridge at Swift Run Gap into the Shenandoah Valley.

Jackson returns his army to the Valley by rail, from Mechum’s River Station through Rockfish Gap to Staunton.

On March 23, 1862, the American army won the first battle at Kernstown, south of Winchester, but Jackson’s aggressiveness caused great alarm in Washington. Believing Jackson outnumbered, Lincoln sent thousands of federal troops back into the Valley. Although this battle was a tactical loss for Jackson, he achieved a strategic victory by keeping the Federals in Richmond.

From Kernstown, Jackson retreated down the valley to Swift Run Gap, where he was reinforced by General Richard Ewell’s division. Meanwhile, American General John C. Fremont moved from present-day West Virginia to threaten the Valley. Leaving Ewell in the valley to oppose Banks’ forces, Jackson tricked the Federals into marching the remainder of his small army east and out of the valley toward Richmond. A day later he secretly moved his troops back into the Valley by rail to Staunton in a counter-offensive. On May 8, Jackson surprised Fremont’s advance guard under General Robert Milroy

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By the end of May, Jackson had 17,000 men in his ranks. He moved them north against Banks’ main force at Strasbourg. Using his knowledge of the valley’s geography, Jackson outflanked Banks by marching the bulk of his army over Massanutten Mountain. The Confederates surprised and overpowered a small Federal outpost at the Battle of Front Royal, at the north end of the Massanutten, on May 23. Banks, finding Jackson in the rear, had no choice but to order a hasty retreat to Winchester, in the hope of holding out there.

Before Banks reached Winchester on May 24, Jackson cut the retreating Federal column on the Valley Turnpike in a fight through Middletown. The Federals at the head of the column continued north to Winchester, and the column behind fled westward out of the valley. Jackson hoped to pursue Banks to Winchester, but some of the Confederate troops began looting the wagons they had captured. This lost momentum allowed the remainder of Banks’ force to reach Winchester safely that night.

To regain his momentum, Jackson attacked Winchester the next morning on May 25. Jackson’s success at the First Battle of Winchester forced Banks to retreat toward Harper’s Ferry and into Maryland. Outnumbered and facing two Union armies, Jackson cleared the Shenandoah Valley of all Union troops in just over two weeks.

Lincoln ordered three Federal columns to assemble in the Valley and capture the Confederates. Jackson marched furiously with his men, hoping to escape the Federal pincers that were massing toward Strasburg. Banks attacked Jackson from behind as Major General John C. Fremont threatened from the west and the forces of American Major General James Shields approached from the east. Jackson’s ragged men barely cleared the town on June 1 as the Federal columns gathered behind them. After their narrow escape, Jackson hurried south down the valley.

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Jackson was about to stop at Port Republic, a small village at the southern end of Massanutten. Jackson’s control of the only bridges spanning the South Fork prevented the two Federal columns from joining. Jackson planned to attack them separately, starting with Fremont. The Battle of the Cross Keys ended at nightfall on June 8. The Confederates maintained control of the field and kept the Federal columns separated.

After halting Fremont’s column at Cross Keys, Jackson turned his attention to the smaller Shield force at the Battle of Port Republic on June 9. Jackson left Ewell at Cross Keys to hold Fremont and concentrated the rest of his army on Shields at Port Republic. Although moving his men from the Cross Keys to Port Republic proved difficult, Jackson won his second battle in two days, ending the spring campaign in the Valley.

The Valley Campaign, March to May 1862: Hal Jesperson’s Battle Map,, shows Jackson’s allies (red) advancing up the Shenandoah Valley, or north, fighting Shields’ Federals (blue) at Kernstown; then Jackson retreats into the valley, or south, to link up with Joel’s troops before moving west into the mountains to fight the Federals at McDowell.

The Valley Campaign, May to June 1862: Hal Jesperson’s battle map,, shows Jackson’s allies (red) entering the Valley from the west, advancing north to engage Bank’s Federals (blue) at Front Royal and Winchester; then head back south to the Cross Keys and Port Republic battles before leaving the valley to the east. View of the Yellowstone Caldera from the Washburn Range. The caldera extends to the base of the Red Mountains in the upper right corner of the photo. The rim of the Grand Canyon of Yellowstone is in the foreground.

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Supervolcanoes are volcanic centers that have experienced eruptions ranked at level 8 on the Volcanic Explosivity Index (VEI). The VEI is a scale that describes the size of volcanic eruptions based on magnitude and intensity. It is a numerical scale (from 0 to 8) on a logarithmic basis that is generally analogous to earthquake magnitude scales.

The volcanic centers (known as reviving calderas) that produced VEI 8 eruptions are truly massive in scale, although they do not build imposing volcanic edifices like shield volcanoes. For example, the Yellowstone caldera is approximately 53 by 28 miles (85 by 45 km) in diameter, but its walls rise only about 1,600 feet (500 m).

VEI 8 eruptions emit so much molten material that the roof of the magma chamber collapses, forming cauldron-like structures known as calderas. The overall landform of a reviving caldera is a broad volcanic plateau surrounded by low cliffs that mark the position of the caldera walls and contains a raised area (re-dome) in the center caused by the movement of magma underground.

Regenerated caldera systems experience many eruptions of varying intensity and magnitude before and after those that create the caldera. Both Yellowstone and Valles Calderas, two reviving calderas in the national parks, have erupted various lava flows, lava domes, and/or pyroclastic material in pre- and/or post-caldera activity.

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Although the term “supervolcano” is established in the popular lexicon, its scientific use is less so. Some volcanologists, including Mike Poland, chief scientist at the Yellowstone Volcano Observatory, don’t like the term. These scientists prefer to describe VEI 8 eruptions as “super eruptions” instead of calling the volcanic centers themselves “super”. Volcanic centers that have VEI 8 eruptions also experience low-magnitude eruptions, both before and after climate caldera formation

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