Lough Talt
Lough Talt is situated in south County Sligo between the villages of Tubbercurry, Aclare and Bonniconlon, in the west of Ireland.
It is the largest of the lakes in the Lough Hoe Bog area.
It is a glacier lake and lies at approximately 500 ft above sea level and measures 67 ft at its deepest point.
It s area is nearly 194 acres.
Lake Columbia
Lake Columbia is a small man- made lake in Columbia Township in southern Jackson County in the U.S. state of Michigan.
Originally formed as a mill pond in 1836, it was expanded to in 1961.
At its greatest extent, the lake is 2 and 1/ 4 miles long and 1 and 3/ 4 miles wide.
It has approximately of shoreline and the water source to the lake is Goose Creek.
The lake has an average depth of.
Lake Columbia is located west of Brooklyn, Michigan.
The latitude for the lake is 42.0928 and the longitude is- 84.3011 with an elevation of above sea level.
Lake Columbia resides in the Columbia School District.
Columbia schools offer a Pre- K through third grade school in Brooklyn called Columbia Lower Elementary( Formerly Brooklyn Elementary).
Grades four through six are at Columbia Upper Elementary( formerly Columbia Middle School).
Grades seven through twelve are at Columbia Central Junior- Senior High School( formerly Columbia Central High School) on Hewitt Road of Lake Columbia.
Also has an alternative high school and adult education program at Columbia Options School which is located in Clark Lake.
Lake Columbia is one of the many lakes in Jackson County that is entirely private.
Yearly membership dues in the Lake Columbia Property Owners Association are required by residents of the lake.
The lake has a total of 16 private parks.
It also has 14 named shores where residents reside.
It is a boaters and fishers paradise for local residents of the lake.
Lake Columbia is stocked annually with Walleye or Bluegill fish.
The fish population continues to grow in Lake Columbia every year.
Hill of Ben
Situated between Lough Glore and Lough Lene, and Lough Ban, Ireland, the Hill of Ben dominates the valley where Fore abbey was built by De Lacy of the Lord of Meath family for the French Benedictine monks.
It rises sharply among the other surrounding hill that interlace with the many loughs of Westmeath.
Local legend has it that Saint Patrick's successor, named Benigne, is said to have preached from the hill to bring the gospel to local communities.
Sligo Way
The Sligo Way is a long- distance trail in County Sligo, Ireland.
It is long and begins in Larrigan, near Lough Talt and ends in Dromahair.
It is typically completed in three days.
It is designated as a National Waymarked Trail by the National Trails Office of the Irish Sports Council and is managed by Sligo County Council, Sligo Integrated Development Company and the Sligo Walks Partnership.
Starting at the shores of Lough Talt, the trail crosses the Ox Mountains, via Lough Easkey, to reach Coolaney and then follows roads to Collooney.
From Collooney, it crosses Union Wood, past Ballygawley Lough, and, entering Slish Woods, follows the shore of Lough Gill to reach the end at Dromahair.
The terrain consists of forest tracks, roads and moorland paths.
A review of the National Waymarked Trails in 2010 found low multiday usage and medium to high day usage of sections of the Sligo Way and recommended the proportion of walking on tarred roads( 51%) be reduced and consideration given to developing the trail as a dual walking and cycling route.
Glacial Lake Columbia
Glacial Lake Columbia was the lake formed on the ice- dammed Columbia River behind the Okanogan lobe of the Cordilleran Ice Sheet when the lobe covered of the Waterville Plateau west of Grand Coulee in central Washington state during the Wisconsin glaciation.
Lake Columbia was a substantially larger version of the modern- day lake behind the Grand Coulee Dam.
Lake Columbia's overflow – the diverted Columbia River – drained first through Foster Coulee, and as the ice dam grew, through first Moses Coulee, and finally, the Grand Coulee.
Kilmactigue
Kilmactigue, is a townland and parish in County Sligo, Ireland.
The parish covers the villages of Aclare, Banada and Tourlestrane, as well as their surrounding townlands.
The parish church is situated in Tourlestrane, and there are smaller churches in Kilmactigue and Lough Talt.
There was also a small church in Banada at the abbey, but it closed when the Banada Abbey secondary school was merged with the Marist Convent secondary school in Tubbercurry.
The parish patron saint is Saint Attracta, who is said to have defeated a dragon that was killing farmers' livestock.
A local well is named after her, as is the new secondary school in Tubbercurry.
Lough Derg (Shannon)
Lough Derg, historically Lough Dergart, is a freshwater lake in the Shannon River Basin, Ireland.
It is the third- biggest on the island of Ireland( after Lough Neagh and Lough Corrib).
It is a long, narrow lake, with shores in counties Clare( south- west), Galway( north- west), and Tipperary( to the east).
It is the southernmost of three large lakes on the River Shannon; the others being Lough Ree and Lough Allen.
Towns and villages on Lough Derg include Portumna, Killaloe& Ballina, Dromineer, Terryglass, Mountshannon and Garrykennedy.
The lake's name evolved from the Irish" Loch Deirgdheirc".
This was one of the names of The Dagda, an Irish god, and literally means" red eye".
Columbia and Sumter Railroad
The Columbia and Sumter Railroad was a South Carolina railroad that operated immediately after the American Civil War.
The Columbia and Sumter Railroad was chartered by the South Carolina General Assembly in 1866.
The line was sold to the Wilmington, Columbia and Augusta Railroad Company in 1870.
The Wilmington, Columbia and Augusta lasted until 1898 when it was absorbed into the Atlantic Coast Line Railroad.
Dry Falls
Dry Falls is a, 5.5 km in width, scalloped precipice with four major alcoves, in central Washington scablands.
This cataract complex is on the opposite side of the Upper Grand Coulee from the Columbia River, and at the head of the Lower Grand Coulee, northern end of Lenore Canyon.
According to the current geological model, catastrophic flooding channeled water at 65 miles per hour through the Upper Grand Coulee and over this rock face at the end of the last ice age.
It is estimated that the falls were five times the width of Niagara, with ten times the flow of all the current rivers in the world combined.
Nearly twenty thousand years ago, as glaciers moved south through North America, an ice sheet dammed the Clark Fork River near Sandpoint, Idaho.
Consequently, a significant portion of western Montana flooded, forming the gigantic Lake Missoula.
About the same time, Glacial Lake Columbia was formed on the ice- dammed Columbia River behind the Okanogan lobe of the Cordilleran Ice Sheet.
Lake Columbia's overflow – the diverted Columbia River – drained first through Moses Coulee and as the ice dam grew, later through the Grand Coulee.
Eventually, water in Lake Missoula rose high enough to float the ice dam until it gave way, and a portion of this cataclysmic flood spilled into Glacial Lake Columbia, and then down the Grand Coulee.
It is generally accepted that this process of ice- damming of the Clark Fork, refilling of Lake Missoula and subsequent cataclysmic flooding happened dozens of times over the years of the last Ice Age.
This sudden flood put parts of Idaho, Washington, and Oregon under hundreds of feet of water in just a few days.
These extraordinary floods greatly enlarged the Grand Coulee and Dry Falls in a short period.
The large plunge pools at the base of Dry Falls were created by these floods.
Once the ice sheet that obstructed the Columbia melted, the river returned to its normal course, leaving the Grand Coulee and the falls dry.
Today, this massive cliff can be viewed from the Dry Falls Interpretive Center, part of Sun Lakes- Dry Falls State Park, and located on Route 17 near the town of Coulee City.
Admission is free, although a Discover Pass is required for parking.
Kingdom, New York
Kingdom is a hamlet located in the towns of Columbia and Warren in Herkimer County, New York.

Question: Are Lough Talt and Lake Columbia located in the same country?
Answer: no