| The Candelabrum | |
| Elevation Ft: | 4700. |
| Elevation Ref: | [1] |
| Prominence Ft: | 80. |
| Isolation Mi: | 0.31 |
| Etymology: | Candelabrum |
| Map: | Utah#USA |
| Country: | United States |
| State: | Utah |
| Region: | Grand |
| Region Type: | County |
| Part Type: | Protected area |
| Part: | Arches National Park |
| Range: | Colorado Plateau |
| Coordinates: | 38.6288°N -109.6°W |
| Topo: | USGS The Windows Section |
| First Ascent: | 1986 |
| Rock: | Entrada Sandstone |
| Age: | Jurassic |
| Easiest Route: | A2 |
The Candelabrum is a 4700feet pillar in Grand County, Utah, United States.
The Candelabrum is located within the Park Avenue section of Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member.[2] Topographic relief is significant as the summit rises 300abbr=offNaNabbr=off above the Park Avenue Trail in 300abbr=offNaNabbr=off laterally. Precipitation runoff from Candelabrum drains to the Colorado River via Courthouse Wash. The first ascent of the summit was made in November 1986 by Charlie Fowler and Chris Goplerud via Play with Fire rock-climbing route.[3] Kyle Copeland and Alison Sheets first climbed the Hall of Flame route in 1986.[4] [5] This landform was shown briefly in the opening scene of the 1989 American action-adventure film Indiana Jones and the Last Crusade.
According to the Köppen climate classification system, The Candelabrum is located in a cold semi-arid climate zone with cold winters and hot summers.[6] Spring and fall are the most favorable seasons to experience Arches National Park, when highs average 60F80F and lows average 30F50F. Summer temperatures often exceed 100F. Winters are cold, with highs averaging 30F50F, and lows averaging 0F20F. As part of a high desert region, it can experience wide daily temperature fluctuations. The park receives an average of less than 10 inches (25 cm) of rain annually.