The clay and mud forming the future shale was eroded from a mountain range that was rich in iron minerals, roughly 400+ million years ago, thus the red color.
plateaus,rivers,lakes,plains,and waterfalls The plains, plateaus, and rivers and lakes are the major landforms of Texas. I would't say waterfalls though. I don't know of any waterfalls in Texas. In Texas there is lots of grazing ground for cattle, therefore, that is why the state sells loads of beef.
The Red sea and the Red river.
No, red tides are not always red. They can appear as a variety of colors including red, brown, green, and even orange. The color of a red tide is influenced by the type of algae present and environmental conditions.
Slate is a fine-grained, foliated metamorphic rock that is formed from the sedimentary rock shale. It is typically gray in color, smooth and easy to split into thin sheets. Slate is commonly used in roofing, flooring, and as a material for billiard tables.
This may not be enough information but the only one I am aware of is the Ruby. Garnets are red too.
Most red shale hills yield an abundant supply of Cyprus trees year-round due to their high level of permeability. Also, in some parts of California, Great Sequoias are found on these hills.
It can be green red black gray brown and yellow. People use it for Oil or natural gas. Shale is the parent rock of Slate. Used for brick ,tile ,pipe ,pottery ,and others.
In the Oxford English Dictionary there is no record of symmone, but there is symon. Symon is a local name for a kind of red shale; it is also attributed to the symon fault -- an interruption of a seam of coal by shale or other material.
276 miles taking this route:Go up to I-69/I-94, and take I-69/I-94 EAST to CANADA via the BLUEWATER BRIDGE (toll bridge).Cross the BLUEWATER BRIDGE (toll bridge) from PORT HURON, MICHIGAN, U.S.A. into SARNIA, ONTARIO, CANADA.From there, continue on HIGHWAY 402 EAST to HIGHWAY 401 EAST at END HIGHWAY 402 near London.Take HIGHWAY 401 EAST to HIGHWAY 403 EAST to NIAGARA FALLS at EXIT 235 near Woodstock.Take HIGHWAY 403 EAST to the LINCOLN M. ALEXANDER PARKWAY at EXIT 64.Take the LINCOLN M. ALEXANDER PARKWAY and the RED HILL VALLEY EXPRESSWAY around Hamilton to the QEW to NIAGARA.Take the QEW NIAGARA to HIGHWAY 405 to QUEENSTON and LEWISTON, U.S.A. at EXIT 37 in the NIAGARA REGION.Take HIGHWAY 405 EAST back to the U.S.A. via the QUEENSTON-LEWISTON BRIDGE (toll bridge).Once you have crossed the QUEENSTON-LEWISTON BRIDGE (toll bridge) and once you have cleared the border, continue on I-190 SOUTH to I-90 via I-290; once you are at I-90, follow signs to I-90 THRUWAY (toll) EAST to ALBANY.Take I-90 New York State THRUWAY (toll) EAST to I-490 EAST to ROCHESTER at EXIT 47.Take I-490 EAST to Rochester.
why dont you go there and find out, I would but I am in the middle of an IT lesson. :)
175 kilometres taking this route:Take HIGHWAY 401 EAST from London to HIGHWAY 403 to NIAGARA FALLS at EXIT 235.Take HIGHWAY 403 EAST to the QEW to NIAGARA via the LINCOLN M. ALEXANDER PARKWAY (EXIT 64 off HIGHWAY 403) and the RED VALLEY EXPRESSWAY to bypass HAMILTON.Take the QEW to St. Catherines.
plateaus,rivers,lakes,plains,and waterfalls The plains, plateaus, and rivers and lakes are the major landforms of Texas. I would't say waterfalls though. I don't know of any waterfalls in Texas. In Texas there is lots of grazing ground for cattle, therefore, that is why the state sells loads of beef.
Some common plants found around Niagara Falls include Eastern red cedar, sugar maple, white pine, and yellow birch. These plants have adapted to the varied conditions of the area, such as mist from the falls and varying moisture levels in the soil. Additionally, native wildflowers like trilliums and violets can also be spotted in the surrounding woodlands.
Schist is more of a texture versus a color. A schist is a type of metamorphic rock. What makes a rock fit into the schist category is the orientation of the mineral crystals in the rock. They can be most any color. A large portion of them are dark in color being black, grey or greenish because of the minerals that exist under metamorphic conditions.
Slate is made up of mostly of quartz and muscovite, often with some biotite, chlorite, and/or hematite. Small quantities of apatite, graphite, kaolin, magnetite, tourmaline, and zircon may also be present in measureable amounts.
There are three main types of slate rock based on their color and composition: black slate, red slate, and green slate. Black slate is the most common type, formed from shale, while red slate gets its color from iron oxide. Green slate is typically formed from chlorite or other minerals containing green pigments.
North Dakota has the Missouri Escarpment which is a slope that the glaciers pushed up and over. The Red River has a very flat river bed from glaciation. There is the Missouri Plateau with holling hills. It has the Turtle Mountains and the Little Missouri Badlands which is very hilly and eroded landscape.