|
The Sunday School Progam materials is form ages 5+ One morning I got up and went outside. As I looked up at my Explorer parked at the front of my house was a spider that came over night and webbed a web up to my front license plate that says Jesus is Lord. That is how the character Hale, got his name in the Jeansus Stories. Hale is the evil one in Jenasus that represents darkness and tried to lore creatures into his web where they think it is just the place to be as bugs seem to dance all night long at Hales home?
If you would like to read more of the Jenasus Childrens Stories and lesson plans for Sunday School simply go to the register page and in the comments place JENASUS. Then Dan will contact you and direct you to the proper pages. You must still fill out the form completely before you submit it. Ted the Turtle Some Characters in Jenasus: Ted the Turtle/ Fron the Frog/ Fred the Frog frons brother/Bobbie the bee/Betty the Butterfly/Chip the Chipmonk/ Moe the mole/Sly the fly/Hale the spider/Stan the stick bug/Daddy Don Longlegs/Albert the ant/ Andy the ant alberts brother/Wilber the wasp/Roe the unfair Erwig/Roger the roach/Lucy the ladybug/Bert the beatle/ Mert the mosquito /Willy the earth worm/ Mr. Wise
The plants in Jenasus are from the Bible. From Mr. Wise the tree that stands tall in over looking Jenasus or the sweet mint, Dill, onions and gralic, Rose of Sharon, ferns, all are for teaching children about God's creation. For a list of plants [ Visit the Rose of Sharon outdoor classroom and prayer garden]
Sandstone surround Jenasus. What is sandstone? Any sedimentary rock composed of stony grains between 1/16 mm and 2 mm in diameter that are cemented together is a sandstone. Sandstone forms from beds of sand laid down under the sea or in low-lying areas on the continents. As a bed of sand subsides into the earth's crust, usually pressed down by over-lying sediments, it is heated and compressed. Hot water flows slowly through the spaces between the sand grains, importing dissolved minerals such as quartz, calcium carbonate, and iron oxide. These minerals crystallize around the sand grains and cement them together into a sandstone. Spaces remain between the grains, resulting in a porous, spongelike matrix through which liquids can flow. Petroleum and natural gas are often found in sandstones. They do not form there, but seek to float to the surface by percolating through water-saturated sandstones. Sandstone layers shaped into domes by folding or other processes (and overlaid by non-porous rock) act as traps for migrating oil and gas, that ascend into them but then have no way out. Such traps are much sought after by oil companies; indeed, most sandstone sedimentologists work for the petroleum industry. Another useful feature of sandstones is that they tend to record the surface conditions that prevailed when their sands were created and deposited. For example, the diagonal laminations often seen running across sandstone beds record the direction and speed of the water or wind that deposited their original sand. Furthermore, the ratio of feldspar to quartz in a sandstone reveals whether its sand was produced by rapid erosion, such as occurs in young, steep mountain ranges, or more slowly, such as occurs in flatter terrain. Since sand beds are often deposited rapidly by wind or water, tracks of reptiles—and even the pocks made by individual raindrops—may be preserved as fossils in sandstone. A sandstone may be uplifted to the surface and broken down by weather into sand. This sand may be deposited in a bed that subsides, turns to sandstone, returns to the surface, breaks down into sand again, and so on. Some individual grains of sand have participated in more than 10 such cycles, each of which lasts on the order of 200 million years.
|
