, 1994, Douglas et al., 1996, Gallart et al., 1994, Dunjó et al., 2003 and Trischitta, 2005), and they symbolize an important European cultural heritage (Varotto, 2008 and Arnaez MK-1775 mw et al., 2011). During the past centuries, the need for cultivable and well-exposed areas determined the extensive anthropogenic terracing of large parts of hillslopes. Several publications have reported the presence, construction, and soil relationship of ancient terraces in the Americas (e.g., Spencer and Hale, 1961, Donkin,

1979, Healy et al., 1983, Beach and Dunning, 1995, Dunning et al., 1998 and Beach et al., 2002). In the arid landscape of south Peru, terrace construction and irrigation techniques used by the Incas continue to be utilized today (Londoño, 2008). In these arid landscapes, selleck chemical pre-Columbian and modern indigenous population developed terraces

and irrigation systems to better manage the adverse environment (Williams, 2002). In the Middle East, thousands of dry-stone terrace walls were constructed in the dry valleys by past societies to capture runoff and floodwaters from local rainfall to enable agriculture in the desert (Ore and Bruins, 2012). In Asia, terracing is a widespread agricultural practice. Since ancient times, one can find terraces in different topographic conditions (e.g., hilly, steep slope mountain landscapes) and used for different crops (e.g., rice, maize, millet, wheat). Examples of these are the new terraces now under construction in the high altitude farmland of Nantou County, Taiwan (Fig. 2). Terracing has supported intensive agriculture in steep Rebamipide hillslopes (Landi, 1989). However, it has introduced relevant geomorphic processes, such as soil erosion and slope failures (Borselli et al., 2006 and Dotterweich, 2013). Most of the historical terraces are of the bench type with stone walls (Fig. 3) and require maintenance because they were built

and maintained by hand (Cots-Folch et al., 2006). According to Sidle et al. (2006) and Bazzoffi and Gardin (2011), poorly designed and maintained terraces represent significant sediment sources. García-Ruiz and Lana-Renault (2011) proposed an interesting review about the hydrological and erosive consequences of farmland and terrace abandonment in Europe, with special reference to the Mediterranean region. These authors highlighted the fact that several bench terraced fields were abandoned during the 20th century, particularly the narrowest terraces that were impossible to work with machinery and those that could only be cultivated with cereals or left as a meadow. Farmland abandonment occurred in many parts of Europe, especially in mountainous areas, as widely reported in the literature (Walther, 1986, García-Ruiz and Lasanta-Martinez, 1990, Harden, 1996, Cerdà, 1997a, Cerdà, 1997b, Kamada and Nakagoshi, 1997, Lasanta et al., 2001 and Romero-Clacerrada and Perry, 2004).