Lake Bull ( ) is a small lake 0.5 nmi east of Lake Vanda in Wright Valley, Victoria Land.
 The name appears to have been applied in the 1960s, probably in association with nearby Bull Pass, or for physicist Colin Bull, for whom the pass is named.
The Onyx River is an Antarctic meltwater stream which flows westward through the Wright Valley from Wright Lower Glacier and Lake Brownworth at the foot of the glacier to Lake Vanda, during the few months of the Antarctic summer.
 Despite being only 32 km in length it is the longest river in Antarctica.
Los Naranjos is the name for an archaeological region in western Honduras.
 It lies on the north border of Lake Yojoa.
 It is significant to the region because of its implications on determining where the Mayan frontier existed, as well as which ancient peoples were in contact and what relations between "tribes" may have been like.
 Whether or not the Maya influenced the people of the Lake Yojoa region is disputed.
Lake Yojoa is the largest lake in Honduras with a surface area of 79 square kilometers (30.50 mi²) and an average depth of 15 meters (50 ft).
 At an altitude of 700 meters (2,300 ft), it lies in a depression formed by volcanoes.
 The Lake Yojoa volcanic field consists of Pleistocene to Holocene scoria cones, craters, and lava flows.
The Wright Valley, named for Sir Charles Wright, is the central one of the three large Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound at approximately .
 Wright Valley contains the Onyx River, the largest river in Antarctica, Lake Brownworth, the origin of Onyx River, and Lake Vanda, which is fed by the Onyx River.
 Its southwestern branch, "South Fork", is the location of Don Juan Pond.
 The upland area known as the Labyrinth is at the valley's west end.
Lake Vanda is a lake in Wright Valley, Victoria Land, Ross Dependency, Antarctica.
 The lake is 5 km long and has a maximum depth of 69 m. On its shore, New Zealand maintained Vanda Station from 1968 to 1995.
 Lake Vanda is a hypersaline lake with a salinity more than ten times that of seawater, more than the salinity of the Dead Sea, and perhaps even more than of Lake Assal (Djibouti), which is the world's most saline lake outside of Antarctica.
 Lake Vanda is also meromictic, which means that the deeper waters of the lake don't mix with the shallower waters.
 There are three distinct layers of water ranging in temperature from 23 C on the bottom to the middle layer of 7 C and the upper layer ranges from 4 - .
 It is only one of the many saline lakes in the ice-free valleys of the Transantarctic Mountains.
 The longest river of Antarctica, Onyx River, flows West, inland, into Lake Vanda.
 There is a meteorological station at the mouth of the river.
Don Juan Pond, also called Don Juan, is a small and very shallow hypersaline lake in the west end of Wright Valley (South Fork), Victoria Land, Antarctica, 9 km west from Lake Vanda.
 It is wedged between the Asgard Range to the south and the Dais Range to the north.
 On the west end is a small tributary and a rock glacier.
 With a salinity level of over 40%, Don Juan Pond is the second saltiest known body of water on Earth.
 This salinity allows the pond to remain liquid even at temperatures as low as -50 C due to the interference of salts with the bonding of water molecules.
Anderson Scarp ( ) is an upward slope and cliff 935 m high, about 0.8 nmi west of Hall Bluff on the Dais, Wright Valley, in the McMurdo Dry Valleys of Antarctica.
 It was named by the Advisory Committee on Antarctic Names in 2004 after Kent Anderson of the Albuquerque Seismological Laboratory, U.S. Geological Survey, from 1992.
 He played a key role in the installation of the VNDA seismograph station at Bull Pass, near Lake Vanda, in the early 1990s.
Lake Canopus is a small lake 65 m above the southern shore of Lake Vanda in Wright Valley, Victoria Land.
 It was named by the Eighth Victoria University of Wellington Antarctic Expedition, 1963–64, after Canopus, pilot of Menelaus, the king of Sparta.
Vanda Station was an Antarctic research base in the western highlands (Victoria Land) of the Ross Dependency, specifically on the shore of Lake Vanda, at the mouth of Onyx River, in the Wright Valley.
 The four original station buildings were constructed in the austral summers of 1967–1968 and 1968–1969, just prior to the first winter-over by a five-man team from January to October 19, 1969.
 Subsequent wintering parties occupied the station in 1970 and 1974.
 During summer seasons, Vanda station was fully staffed until 1991.
 Scientific programs principally included meteorology, hydrology, seismology, earth currents, and magnetics.
 The station was administered by the Department of Scientific and Industrial Research (DSIR), and was supported logistically by the permanent New Zealand research base of Scott Base on Ross Island.

Question: Is the Honduran Lake Yojoa deeper on average than Antartica's Lake Vanda?
Answer: no