Nowadays, Mount Talbert is a topic that has gained great relevance in modern society. With the advancement of technology and globalization, Mount Talbert has become a topic of interest to many people around the world. From its impact on the economy to its influence on culture and politics, Mount Talbert is an aspect that cannot be overlooked. In this article, we will explore different aspects related to Mount Talbert and its role in today's society. From its origins to its evolution over time, we will closely analyze the impact that Mount Talbert has had in various areas, as well as the possible implications it could have in the future.
| Mount Talbert | |
|---|---|
| Highest point | |
| Elevation | 740+ ft (230+ m) NGVD 29[1] |
| Prominence | 410 ft (120 m)[1] |
| Coordinates | 45°25′36″N 122°33′06″W / 45.4267871°N 122.5517579°W[2] |
| Geography | |
| Parent range | Cascade Range |
| Topo map | USGS Gladstone |
| Geology | |
| Volcanic field | Boring Lava Field |
| Last eruption | 500,000 years ago[3] |
Mount Talbert is a volcanic cinder cone in Clackamas County, Oregon. It is part of the Boring Lava Field,[3] a zone of ancient volcanic activity in the area around Portland. Its summit rises to an elevation of 740+ ft (230+ m).
The butte remains undeveloped and is the location of a nature park of the same name which is managed by North Clackamas Parks & Recreation District. The park has 4.2 miles (6.8 km) of hiking trails, including Park Loop, Summit and West Ridge Trail, along which there are several instructive signs about the area's natural resources.
In 2005 the recreation district began promoting regrowth of more fire resistant white oak by girdling and removing Douglas firs, which impede the growth of the oaks by shading out the sun.[4]