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The COMPLETE land lease record contains in most cases the land lease petition and possible supporting documents that may include valuable information about the petitioner and his or her family.
The miscellaneous petitions (dating from 1780's) are a real grab-bag of information, you never know what may turn up here.
Birds at Jefferson include mallards, northern goshawks, sharp-shinned hawks, red-tailed hawks, dusky grouses, grey partridges, killdeers, spotted sandpipers, California gulls, band-tailed pigeons, great horned owls, mountain pygmy owls, common nighthawks, rufous hummingbirds, Northern flickers, pileated woodpeckers, yellow-bellied sapsuckers, hairy woodpeckers, and white-headed woodpeckers.
Some documents are extremely lengthy, but most petitions are less than 5 pages. township) within the general County or District locations recorded in the following index. The reproduction, copying, downloading, storage, recording, broadcasting, retransmission and distribution of any part of these pages (including all text, compilations, graphics and source code) without the written permission of Michael Stephenson is strictly prohibited.
Mount Jefferson is a stratovolcano in the Cascade Volcanic Arc, part of the Cascade Range in the U. Due to the ruggedness of its surroundings, the mountain is one of the hardest volcanoes to reach in the Cascades.
These extensional processes formed grabens, or valley-like depressions between parallel fault lines, at the eastern boundary of the central Cascades, including a 4,000-foot (1,200 m) deep formation.
Jefferson does not lie in one of these grabens, but these tectonic processes continue, albeit at a less dramatic rate.
The Whitewater Glacier and the northeastern side of the volcano drain into the Whitewater River, and the Shitike Creek flows between Mount Jefferson and Olallie Butte before reaching the Deschutes River.
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Vegetation at Mount Jefferson is dominated by Douglas-fir, silver fir, mountain hemlock, ponderosa pine, lodgepole pine, and several species of cedar.Mount Jefferson lies in the temperate maritime climate of Western Oregon.The Cascades absorb east-moving moisture, causing warm and dry summers.The flood on August 21, 1934, at a lake formed near Whitewater Glacier, created a debris flow that reached the Whitewater River drainage and buried parts of Jefferson Park in 1 to 8 feet (0.30 to 2.44 m) of debris; another event took place in 1957, but was poorly documented.Mount Jefferson has 35 snow and ice features, including four named glaciers: Whitewater, Jefferson Park, Russell, and Waldo.Civilian petitioners sometimes indicated their country or place of origin. Further information that may be found in some of the petitions includes arrival date in Canada, previous residence, date and place of birth, age, marital status and names of other family members, oaths of allegiance, and character references. These features, for the most part on the northern, eastern, and southeastern parts of Mount Jefferson, span elevations from 6,158 to 8,189 feet (1,877 to 2,496 m) and cover an area of 2.1 square miles (5.5 km In recent years, the glaciers have retreated to form lateral moraines; Whitewater Glacier, for example, shrunk from 5 miles (8.0 km) in width and 1 to 2 miles (1.6 to 3.2 km) in length to 1.9 miles (3.1 km) in width and a length of 0.62 miles (1 km).During the 20th century, scientists thought they had identified a new glacier, which they named Milk Creek Glacier, but later studies established that it was an artifact of stagnant ice that had been hidden by debris, and it is no longer considered its own distinct feature.The following database has been constructed from the Upper Canada (Ontario) land leases and miscellaneous petitions. Each record in my index consists of the name of the petitioner (maiden names or additional petitioners may be in brackets), the location of the petitioner, and year of the petition.