Monday, April 10, 2017

FLU VIRUS!!!!!!!

HEY EVERYONE!!!!

Sorry if this email is a little short but I have caught a flu virus and I am not feeling too well at the moment but I do have some sweet pics for you guys to make up for it.

On Monday last week we went up to Tobermory and hiked along the coast next to the lake and it was super beautiful. I even drank out of the lake up there because the water is super clean and drinkable. It was a good thing to experience and I wish I had more time to go back and hike it again.

The rest of the week was just a pretty regular week nothing too exciting.

On Saturday this week we have a lady named Joan getting baptized! I am super excited for her and I know how much this is truly going to bless her life.

I love you all so much and wish the best of luck to you this coming week.
--

Elder Murray


Here is a little history on the area that we hiked :
This shoreline marks the northern extremity of the Niagara Escarpment in southern Ontario. Stretching unbroken for 465 miles across southern Ontario from Niagara Falls. The escarpment was created by erosion of layered sedimentary rocks deposited in ancient seas of the Paleozoic Era over 400 million years ago. Portions of the escarpment form the islands between Tobermory and South Baymouth and the same Paleozolic rocks shape the geology of Manitoulin Island. The rock of the escarpment is very old. Approximately 400 million years ago, this area was covered by a shallow tropical sea teeming with life in the form of plant-like animals, crustaceans, living corals and mollusks. It would have looked much like the present-day Great Barrier Reef of Australia. When the sea began to dry up, the minerals dissolved in it became more and more concentrated. Magnesium in the water was absorbed into the limestone, which then became a softer, slightly different sort of rock, called dolomite. Where erosion has cut more deeply, caves have been formed, such as the famed "Grotto" on the shore between the Marr Lake and Georgian Bay Trails. Great blocks of dolomite, undercut by wave action, have tumbled from the cliffs above and can be clearly seen below the surface of the deep, clean waters of Georgian Bay.




 







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