Chapter 128 Yellowstone day 2

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Jossalyn's POV:

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Jossalyn's POV:

The next morning Jossalyn and Chase  wake up when the alarm goes off.

"Hey sorry we are getting up so early but we want to have breakfast and then start our second day here." Chase  says.

"Okay baby." Jossalyn says.

"Are you okay?" Chase  asks.

"Yes I am fine, I promise." Jossalyn  says.

"Okay.  How are the twins doing?" Chase  asks.

"Great these little ones are angels.   I have not been sick anymore." Jossalyn says.

"Good baby I am glad." Chase  says.

"Yes and I am over 16 weeks pregnant so out of my first trimester and into my second so that is good." Jossalyn  replies.

"I am glad baby." Chase  says kissing her head.

They both get up and get dressed.   They then head downstairs.   Everyone meets down there.   Evelyn had made them breakfast sandwiches.   They eat and then Ryan  takes the wheel and drives them to their first stop of the day.    They drive to Artist Point and park, then hit the South Rim Trail along the Grand Canyon of the Yellowstone.     

" The Grand Canyon of the Yellowstone River expresses the park's complex geologic history in dramatic colors and shapes.   Puffs of steam mark hydrothermal features in the canyon's walls.   The Upper and Lower Falls of the Yellowstone River add to the grandeur of the unique natural treasure.    Experience the canyon from a variety of overlooks, at different times of day, and at different seasons. A number of trails and walkways wind along the rims and down partway into the canyon." Jossalyn  reads on the sign.

"About 640,000 years ago, a huge volcanic eruption occurred in Yellowstone, emptying a large underground chamber of magma (partially molten rock). Volcanic ash spread for thousands of miles. The roof of this chamber slowly collapsed, forming a giant caldera 30 miles (45 km) across, 45 miles (75 km) long. The caldera began to fill with lava and sediments. Infilling of lava flows continued for hundreds and thousands of years.    Scientists think the oldest Grand Canyon of the Yellowstone formed in rock and sediments about 160,000 to 140,000 years ago. This paleocanyon was not as deep, wide or long as the canyon you see now." Gianna  continues.

"Past and current hydrothermal activity altered and weakened the rhyolite, making the rocks softer. The Yellowstone River eroded these weakened rocks to deepen and widen the canyon, a process that continues today. The current canyon begins at Lower Falls and ends downstream from Tower Fall." Willow  says.

"The 308-foot (93 m) Lower Falls may have formed because the river flows over volcanic rock more resistant to erosion than the downstream rocks, which are hydrothermally altered. The 109-foot (33 m) Upper Falls flows over similar rocks. The large rocks upstream from Upper Falls are remnants of a lava flow resistant to erosion." Evelyn  continues

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