The peninsula lies east of the Isthmus of Tehuantepeca northwestern geographic partition separating the region of Central America from the rest of North America.
The Yucatan Penisula It has been suggested that the Yucatan Peninsula was the land northward and that at some time in the past the sea extended farther inland creating a neck between the peninsula and the mainland of Central America.
This would create the correct north-south alignment as described in the Book of Mormon and Yucatan definitely has a great deal of favorable archeology to recommend it.
However, there are a number of problems related to this proposal. First, there is no evidence that there ever was a "narrow neck" at the base of Yucatan.
A theory which requires a change in geography is suspect and should be regarded with caution. There are seas as required by the text, however, there does not seem to be a place where the "sea divides the land".
Third, the Yucatan Penisula would be a very limited "land northward" and would not have contained the tremendous Nephite emigration that the book describes.
Also, there are few if any of the older Olmec era sites located on the penisula, most of the ruins being from the classical Maya period.
Fourth, there is no evidence of the geological changes described in the text for the land northward, which took place at the time of the crucifixion.THE YUCÁTAN PENINSULA is made up of three states: Campeche, Quintana Roo, and Yucatán, which also include major resort areas such as Cancún, Cozumel, and Playa del Carmen.
The Yucatán Peninsula extends northward from Central America and is bordered on the east by the CARIBBEAN SEA and on the north and west of the peninsula by the Gulf of Mexico. Many of the peninsula's fine beaches and archaeological sites have been developed for tourism, which is a significant part of the peninsula's economy.
By the early years of the 21st cent. resort development in Mexico on the peninsula's E coast was extensive, especially at Cancún and to its south along cmi ( km) stretch of beach.
Yucatan Peninsula Topography, Climate, and Vegetation The Yucatán Peninsula is a low, undulating, limestone platform that is still gradually emerging from the sea.
lausannecongress2018.comn Peninsula-Rainfall dissolves the limestone bedrock, producing underground caverns. that sometimes.
collapse, forming. sinkholes. Mayan ruins attract tourists and archaeologists.
Section 1 Review. The geological instability of the central plateau. a) is slowly dividing the plateau in half.
b) produces dangerous volcanoes and earthquakes. The Yucatan Peninsula, which includes the Mexican states of Yucatan, Campeche and Quintana Roo, but also a part of Belize and Guatemala, has a tropical climate, with a rainy and muggy season from June to October, a relatively cool season from November to February, and a hot season from March to May, when the highest temperatures of the year are reached, with peaks of more than 40 °C ( °F).
A sinkhole is a natural hole that forms in the Earth's surface as a result of the chemical weathering of carbonate rocks like limestone, as well as salt beds or rocks that can be severely weathered as water runs through them.
The type of landscape made up of these rocks is known as karst topography and is dominated by sinkholes, internal drainage, and caves.