Point Lobos in the context of "Colonial organism"

In biology, a colony is composed of two or more conspecific individuals living in close association with, or connected to, one another. This association is usually for mutual benefit such as stronger defense or the ability to attack bigger prey.

Colonies can form in various shapes and ways depending on the organism involved. For instance, the bacterial colony is a cluster of identical cells (clones). These colonies often form and grow on the surface of (or within) a solid medium, usually derived from a single parent cell.

Conglomerate (/kənˈɡlɒmərət/) is a sedimentary rock made up of rounded gravel-sized pieces of rock surrounded by finer-grained sediments (such as sand, silt, or clay). The larger fragments within conglomerate are called clasts, while the finer sediment surrounding the clasts is called the matrix. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay.

Conglomerates form when rounded gravels deposited by water or glaciers become solidified and cemented by pressure over time. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. They are closely related to sandstones in origin, and exhibit many of the same types of sedimentary structures, such as tabular and trough cross-bedding and graded bedding.

Carmel Highlands is an unincorporated community in Monterey County, California, United States. It is 3.5 miles (5.6 km) south of Carmel-by-the-Sea (better known as simply, "Carmel"), at an elevation of 318 feet (97 m). Carmel Highlands is just south of the Point Lobos State Reserve, and serves as the northern gateway of the Big Sur coastline along California State Route 1. Carmel Highlands was laid out in 1916 by developers Frank Hubbard Powers and James Franklin Devendorf and the Carmel Development Company.